- )*** ., 2004). (Godard, 2001) ( ) - , -. , -
|
|
- Chad Todd
- 5 years ago
- Views:
Transcription
1 .. *,.. **,.. * ( -)*** -. (Godard, 2001), , -. -,, - ( ), -, - (Escola, 1921; Lappin, Smith, 1978.). - -, - - -, (Griffin, 1987). -, (Chopin, 2003).,, - -, -, - *,. **,,. *** ( ). (., 2004). - () -, - (, 1971;, 1974; Pognante, 1985; Mørk, 1986; Koons et al., 1987; Wayte et al., 1989; John, Schenk, ). -, - -. in situ,,, (, 1968), -, - -. () - (, 1990), - (., 2004;, -, 2005;., 2005),,, - -, -, , -, - -- (-, 1990). 37
2 - -, - (. ) , , - - (., 2004) (. 1). ; -,, -, ;, -, -,, ---,. 2720±8 (., 2003) -, - - -, -.,,. 1. () () (.. :., 2006): : 1 (2,5 1,92 ) ; 2 5 : 2 ; 3 ; 4 - ; 5 - (); 6 (2,9 2,7 ); 7 (3,2 2,7 ) ; 8 ; : 1 ( 2,7 ); 2 ; (, ),, -- - ; 4 - ; 5 ; 6 ; 7 - (., 2004); 8,. 38
3 ,, , - -,., ,3±8,1 (., 2004). I, - (Fe-Ti), (Fe) (Na+K, Fe)., -., -, - --,, -, - (. )., -, -. --,, ( Grt * Omp ; = C, = 16,5 17,5 ) -, - --.,, - (20% Jd) (. ). -, - 2,7 2,45, - * : Ab, Act-Hbl, Alm, Am, An, Bt, Cpx, Crn, Di, Ed, Ed-Hbl, En, Fa, Gln, Grt, Grs, Hbl, Jd, Ky, Ne, Ol, Omp, Opx, Pl, Prg, Prg-Hbl, Prp, Qtz, Rut, Sil, Spl, Sps, Uv. Omp Di Jd, Pl An, En, Ol Opx, Grt Prp, Grs., II, (Mg-Cr) -, - - (, 1981). -, 2,43 2, (., 2001;., 2004; Lobach-Zhuchenko et al., 1998),. II -. (. ).. U-Pb ,1±1,3 (-., 2003).. III, - II, - (, -, 2005). - (Fe-Ti) 2,12 (., 2003). - () -. (Fe). -, N-MORB (,, 2005), - - -,, -. - Grt 25 Omp Rut ( = C, = 13,5 14,0 ) III (Fe) - II (Mg-Cr) (. -,. ). -,, II -,. - -.,, -,, -.., : 1),,, I II (. 2, ), III - (.,. 2,,. ) 39
4 ɚ ɛ ɜ ɝ ". 2:, ( $# Q# &' % 7 & 50 ' (( &- & %& II ( &. &##& ) ' (( & III (( &. & &% + 6 ) &7 "% 50 ' 8 $ 3 6 &/ 5 # 3 &"%& & ) ( ) &"%& & ) (() " '& 5) 7& ), 3 Q%&) ' (( & 5 )> (& %5 Q &#& % #%& 50 7& 0 % #%& 7 & 5;, ' Q &#& % #%& 5 7& 5 )> (& 7 8 $# 0 ' (( &- & %& II ( &. & &% + 6 ; ' &. &##& ). J $ ; 2) ' # 5 6 (. 2, )*,. %,, $ () #. * (20 1 ) ($ ) ' #, ', $ #, (. 2, ).! II III ( - \ ;, * ; ) ', ' #.! # ' # II #,. * #, ' # #. W,, #, '. +-4 ' #. * ', Cpx-Pl, $ Jd Omp 20 36%, $ 38 48%. /. ]. * J. * ; II ' $. / ' I III #. 40
5 (. ) ( ): 1 4 : (1) - (2); (I ); 4 ; : ( ); 6 () ( ); 7 8 : 7 - ; 8 ; 9 «-» - ; 10 ; 11 ; 12, ; 13 ; 14 ; 15 ; 16 ; 17 - () (); 18 : () (); 19 :, ~25, , -- (. 3).,, -,.., - -,,. -, ,. -,, - ± -,. - «-», -, - (. 4, )
6 . 4. () (). -31 () ()., (. 4, ) -,,, -, Cpx (Di ),. - -.,, (. 3). -, -, -. -, - (. 3)., (. 2). ( ) - -., -.,, - (±, ). -,,, -, - ( ) -., (. -16/67),, - (, 1981),, Na 2 O (. 1). -,, -. -., - - (. 3). - (7 8 ) - (8 10 ). (. 3) - -, I (. 1). - 33% Jd, - (- ),, -, , -, (. -49). 42
7 1 : (II ); 7 8 (I ) / #Mg 78,19 75,24 77,04 74,07 73,27 73,14 47,50 50,17 SiO 2 48,10 49,40 49,00 48,90 48,62 48,70 48,08 47,74 TiO 2 0,57 0,62 0,49 0,65 0,71 0,53 1,27 1,15 Al 2 O 3 8,82 10,10 10,20 10,52 9,50 12,00 14,90 15,25 Fe 2 O 3 1,10 1,70 2,50 1,70 2,09 2,46 3,30 2,56 FeO 9,40 8,85 7,67 9,15 9,94 7,80 11,25 10,90 MnO 0,188 0,185 0,178 0,190 0,183 0,172 0,227 0,214 MgO 20,90 17,70 18,68 17,12 18,18 15,30 7,22 7,46 CaO 8,22 8,80 8,53 8,82 7,50 8,98 9,53 9,52 Na 2 O 1,20 1,46 1,46 1,47 1,32 1,85 2,22 2,67 K 2 O 0,32 0,35 0,32 0,31 0,70 0,44 0,40 0,67 H 2 O 0,07 0,02 0,10 0,17 0,20 0,31 0,13 0,21 0,93 0,76 0,68 0,85 0,84 1,00 1,09 1,46 P 2 O 5 0,07 0,07 0,05 0,07 0,09 0,08 0,18 0,14 99,89 100,02 99,86 99,92 99,87 99,62 99,80 99, (. 3): 1 ; 2, 3 - () ; 4 6 : (-33, -49) - (-16/67); 7 8 Mg = MgO/(MgO+Fe)100 (. -). - (. -30, ) - (. 3)., -, - () Cpx (. 2, - 1) - (. 5). - Ol (20% Fa) Spl ( : 49%, 29%, 14% 9%) - Opx (En ), - Am Cr 2 O 3 (1,33. %) Ed-Hbl (. 2,. 5). - Opx, Am - Omp. Cpx Di Jd 12%, - Omp (28% Jd). Omp 35 41% Jd. Omp Cr 2 O 3, - Di-Omp - Cr 2 O 3, 1%. Grt - 49,3% Prp 11,9% Grs (. 2,. 20). Opx (. 2, - 2;. 6, ),,. Opx, Cpx, - Al 2 O 3 (1,03 2,72. %) CaO (2,36 2,39. %). Omp 23,6 40,9% Jd. Grt (Prp 48,4 50,6%, Grs 14,5 17,2%) Omp 46 - (F = 10,4%) (3,29. %) Bt. Omp 38 55% Jd Crn (. 2,. 6, ). Omp Jd (44% 38%) Crn Pl (15,6 17,9% An). -, - (. 6, ). Omp -, Grt Omp 57 Crn, - Omp 5137% Jd Pl 15 Crn., 48, Grt 13 Omp - (30 38% Jd), - (. 7, ) Grt (Prp 4146%, Grs 2315%) (. 3,. 42, 43,. 2, , ),, -,, - ( ). (-30) - Cpx Jd (19 20%), Opx (En 18 ) Am Ed-Hbl Prg-Hbl. - Opx Grt (. 7, )
8 2 - (. -30, ) (. ) , * Di Ed Hbl Opx Opx Ol Spl Opx Di Di Di (Opx) Di Omp Di Omp Omp Omp Omp Omp Grt SiO 2 53,80 46,20 55,76 55,71 38,96 0,22 56,13 54,18 54,31 55,19 55,26 54,28 53,43 54,07 54,98 54,53 52,34 55,23 55,82 40,37 TiO 2 0,13 1,65 0,10 0,10 0,04 0,14 0,07 0,17 0,06 0,21 0,39 0,18 0,2 0,19 0,17 0,17 0,44 Al 2 O 3 2,83 12,39 0,93 0,57 25,85 0,61 2,60 2,94 3,65 0,59 3,60 4,95 4,07 6,20 6,68 13,46 8,83 8,28 22,56 Cr 2 O 3 0,95 1,31 0,16 0,14 35,87 0,63 1,09 1,18 0,06 1,22 0,74 0,94 0,94 0,79 0,03 0,25 0,48 0,07 FeO* 3,75 5,93 12,45 12,21 18,99 31,06 12,53 4,14 4,01 3,69 13,19 4,17 4,23 4,03 3,32 3,65 5,91 3,68 3,43 18,31 MnO 0,09 0,1 0,06 0,12 0,36 0,14 0,07 0,06 0,16 0,12 0,14 0,49 MgO 15,01 16,62 30,03 30,81 41,59 5,73 30,41 14,49 14,41 13,39 30,05 13,98 13,84 13,43 11,72 11,34 10,23 10,78 10,60 13,50 CaO 21,15 11,83 0,51 0,20 0,15 0,28 21,39 20,64 19,88 0,28 19,24 19,51 20,22 17,89 18,11 11,56 15,44 15,48 4,53 NiO / / / / / / / / / 0,18 / / / 0,37 0,02 Na 2 O 2,28 3,39 0,24 0,45 0,66 2,21 2,30 2,72 0,34 2,92 2,85 3,06 4,55 4,57 5,94 5,25 5,44 0,09 K 2 O 0,02 0,59 0,01 0,04 0,01 0,04 0,05 0,02 0,01 0,09 100,01 100,01 100,00 100,01 99,99 100,00 100,00 99,96 99,85 99,87 99,89 100,00 99,99 100,00 99,80 100,00 99,78 100,00 100,00 100,01 Prp 49,3 Alm 37,7 Sps 1,0 Grs 11,9 Uv 0,1 F 12,3 16,7 18,9 18,2 20,4 18,8 13,8 13,5 13,4 19,7 14,3 14,7 14,4 13,8 15,2 24,5 16,1 15,4 43,4 An, % Jd, % 12,0 11,1 12,6 15,7 15,3 20,2 17,3 26,2 28,2 40,9 36,3 35, , Opx Opx Omp Omp Grt Omp Bt Grt Omp Grt Crn Omp Omp Omp (Omp + Omp ) + (Pl + Pl ) SiO 2 56,44 54,48 55,74 55,26 40,40 54,63 40,77 40,89 53,38 40,45 1,22 55,21 54,58 55,66 54,68 54,11 64,79 63,86 TiO 2 0,18 0,07 0,06 3,29 0,14 0,02 0,05 0,26 0,16 0,21 0,19 Al 2 O 3 1,03 2,72 5,54 10,34 22,65 12,87 17,86 22,63 12,53 22,69 97,69 14,09 14,01 15,46 12,34 11,92 22,11 21,94 Cr 2 O 3 0,25 1,08 0,86 0,29 0,13 0,06 0,01 0,06 0,16 0,06 0,01 0,03 FeO* 9,37 10,45 3,38 3,60 16,19 3,05 4,70 16,28 3,26 17,07 0,41 2,61 2,27 2,45 2,64 2,64 0,13 MnO 0,17 0,14 0,01 0,55 0,05 0,18 0,37 0,49 0,01 0,04 0,01 0,10 0,12 0,06 0,08 MgO 30,11 27,95 12,40 9,53 13,18 8,67 22,68 13,84 9,49 13,74 0,33 7,54 8,42 7,18 9,00 9,85 0,15 CaO 2,39 2,36 17,98 14,82 6,57 13,88 0,03 5,69 15,67 5,53 0,31 13,36 12,99 10,98 14,56 15,68 3,22 3,92 NiO 0,13 0,22 / / / / / / / 0,08 0,04 / / / 0,15 / Na 2 O 0,27 0,64 3,96 5,91 0,21 6,72 0,73 0,29 5,54 6,95 7,21 8,01 6,40 5,54 9,52 9,84 K 2 O 0,03 0,02 0,06 9,76 0,01 0,04 0,01 0,05 0,01 0,12 0,13 100,03 100,00 100,02 100,00 100,01 99,99 100,01 100,00 100,01 100,01 100,00 99,99 100,00 100,00 100,01 100,00 100,00 100,00 Prp 48,4 50,6 49,8 Alm 33,3 33,7 34,7 Sps 1,0 0,7 1,0 Grs 17,2 15,0 14,5 Uv 0,1 F 14,8 17,4 13,3 17,5 40,8 16,5 10,4 39,9 16,1 41,0 16,3 13,0 16,1 14,1 13,1 An, % 15,6 17,9 Jd, % 23,6 40,9 46,0 38,3 47,6 49,3 54,5 44,0 38, , , Omp Grt Omp Grt Grt Ed-Hbl Di-Omp Opx Prg-Hbl Di-Omp Prg-Hbl Opx Grt /3 SiO 2 54,87 40,24 55,04 39,67 40,39 46,75 55,14 56,30 45,71 54,49 46,52 55,98 40,07 TiO 2 0,08 0,11 0,03 1,45 0,07 1,44 0,18 0,92 0,03 0,02 Al 2 O 3 7,80 22,64 9,08 22,55 22,53 13,79 4,59 0,65 14,02 4,41 13,84 0,60 22,64 Cr 2 O 3 0,06 0,01 0,05 0,59 0,13 0,03 0,48 0,28 0,37 0,06 FeO* 4,13 18,12 4,25 17,01 18,49 5,95 3,89 12,20 5,89 3,89 5,88 11,94 18,32 MnO 0,56 0,03 0,51 0,42 0,16 0,13 0,06 0,17 0,16 0,63 MgO 11,60 13,08 10,40 11,22 12,55 16,37 13,54 30,48 16,87 13,83 17,09 30,79 13,43 CaO 17,23 5,01 15,41 8,81 5,59 10,02 19,63 0,34 10,47 19,58 9,96 0,24 4,71 NiO 0,07 / 0,21 / 0,19 / / Na 2 O 4,25 0,35 5,67 0,17 4,16 2,80 3,95 3,28 4,28 0,23 0,12 K 2 O 0,02 0,01 0,02 0,84 0,04 0,02 0,84 0,79 0,04 0,02 100,02 100,02 100,00 100,00 100,02 99,99 99,99 100,02 100,01 100,00 100,01 100,01 100,02 Prp 48,1 41,0 46,0 49,0 Alm 37,4 34,7 38,1 37,5 Sps 1,3 1,0 1,0 1,3 Grs 13,2 23,3 14,9 12,2 Uv F 16,7 43,8 18,7 45,9 45,3 16,9 13,8 18,3 16,4 13,6 16,2 17,9 43,4 An, % Jd, % 29,5 38,1 19,5 18,7 44
9 , , Grt Omp Omp Omp Pl Ol Ol Opx Di Grt Grt Grt Omp Di Opx SiO 2 40,00 55,30 54,54 53,52 64,64 39,42 38,47 56,10 54,27 40,22 40,24 40,54 53,88 54,47 55,59 TiO 2 0,02 0,18 0,30 0,22 0,04 0,13 0,10 Al 2 O 3 22,80 15,83 13,98 12,77 22,36 0,79 1,04 22,66 22,86 23,01 12,39 2,29 1,70 Cr 2 O 3 0,01 0,02 0,06 0,04 0,06 0,03 0,12 0,01 0,08 FeO* 18,92 3,30 3,32 3,16 0,02 16,86 18,92 11,58 3,30 17,51 15,63 16,29 2,75 3,05 10,46 MnO 0,44 0,08 0,09 0,12 0,15 0,13 0,03 0,07 0,45 0,24 0,45 0,09 0,11 MgO 12,05 6,71 7,99 9,47 43,48 42,31 31,09 16,65 13,68 12,54 14,23 9,71 16,01 31,74 CaO 5,68 10,20 12,37 15,43 3,13 0,05 0,21 24,33 5,28 8,36 5,48 15,82 22,81 0,18 Na 2 O 0,10 8,39 7,40 5,29 9,63 0,10 0,13 0,34 0,04 0,13 5,23 1,21 0,21 K 2 O 0,03 0,16 0,02 0,01 0,05 0,01 100,01 100,00 100,01 100,01 100,00 100,00 100,01 100,01 100,00 100,01 100,01 100,01 100,00 100,02 100,00 Prp 44,7 49,7 45,5 51,7 Alm 39,3 35,5 32,0 33,1 Sps 1,0 1,0 0,7 1,0 Grs 15,0 13,7 21,8 14,2 Uv 0,1 F 46,8 21,6 18,9 15,8 18,0 20,2 17,3 10,0 41,7 41,3 39,1 13,6 9,7 15,6 An, % 15,1 Jd, % 57,0 50,5 36,6 2,4 36,0 8, : CamScan 4DV Link AN ( ), CamScan MV 2300 ( ) ( , -53). FeO* FeO; F = Fe/(Fe+Mg) 100; An, % = Ca/(Ca+Na+K) 100. : Morimoto, 1988, : Leak, Jd, %, Cpx c : Cawthorn, Collerson, PX (Cebria, 1990). :,,,, - -,,,,,,,.. 5. Cpx - - Ol Spl, Opx - Ed-Hbl ( ). - - (). Jd- Cpx %
10 ". 6. & &"%!4 Q# &' % 7 & + % #6)6 6" + / "%! & & &'& ' (( &- & %. Opx # (24 41% Jd) ( ). * : Grt15 17 Omp38-46 Bt o - # (38 55% Jd) Crn o # (44 38% Jd)- (16 18% An) Crn ( *-30); 45 ' Grt15 Omp57 Crn o # (51 37% Jd)- (15% An) Crn ( *-16-3). \ $ $ ' " %& 5 Q# &' %5 8 %! &$ 7& 5: ' 48 ( Grt 13 Omp30-38) - ; ' Omp19-20 Opx Hbl). *-30. \ $ $ ' ( Grt 12? -
11 3 () Omp Opx Spl Spl Opx Di Prg-Hbl Omp Omp Grt Omp Pl Bt Ed-Hbl Opx SiO 2 54,84 55,26 0,08 0,11 56,00 53,91 45,26 54,53 54,79 40,25 54,35 63,40 39,36 46,33 55,26 TiO 2 0,09 0,09 0,03 0,21 0,24 2,07 0,04 0,10 0,11 0,11 6,57 2,99 0,05 Al 2 O 3 4,52 1,20 10,77 11,99 0,93 3,97 12,19 4,58 5,15 22,13 4,52 22,65 15,77 11,47 0,70 Cr 2 O 3 2,43 0,38 52,10 50,26 0,19 1,42 2,11 1,17 0,16 0,03 0,66 0,30 0,05 FeO* 3,87 12,66 31,95 32,32 12,97 3,84 6,51 3,99 4,27 18,21 4,22 0,22 8,25 7,35 13,25 MnO 0,09 0,17 0,14 0,11 0,17 0,02 0,09 0,55 0,01 0,06 MgO 12,50 29,80 3,45 3,75 29,15 13,99 15,45 13,32 12,93 12,51 13,72 18,76 16,20 30,02 CaO 18,04 0,22 0,10 0,07 0,23 20,02 11,62 18,90 18,78 5,53 19,59 4,17 0,06 11,64 0,22 Na 2 O 3,63 0,38 0,27 0,04 0,43 2,41 3,53 3,13 3,52 0,64 3,30 9,40 0,58 2,98 0,10 K 2 O 0,02 0,05 1,14 0,03 0,04 9,77 0,74 0,02 100,01 100,01 98,92 98,89 100,01 100,02 99,90 99,62 99,73 99,95 99,85 99,99 99,78 100,00 99,73 Prp 46,5 Alm 37,9 Sps 1,0 Grs 14,6 Uv F 14,8 19,3 20,0 13,3 19,1 14,4 15,7 44,9 14,7 19,8 20,3 19,8 An, % 19,7 Jd, % 19,3 17,0 19,6 21,9 19, Di Di Opx Opx Omp Opx Grt Omp Grt Bt Di Grt Grt Grt Pl SiO 2 53,56 54,22 54,96 55,33 54,58 55,16 39,90 55,25 39,55 41,14 53,56 39,86 40,27 39,53 60,96 TiO 2 0,34 0,08 0,03 0,14 0,10 3,50 0,17 0,01 0,01 Al 2 O 3 3,60 4,14 0,93 0,77 4,72 1,11 21,92 5,15 22,51 16,80 5,24 22,35 22,49 22,12 23,91 Cr 2 O 3 1,24 1,21 0,34 0,17 1,10 0,13 0,23 0,10 0,40 0,28 0,09 0,02 FeO* 6,54 4,45 15,00 14,30 4,02 14,70 20,02 4,70 19,33 6,60 4,47 19,15 19,14 20,14 0,27 MnO 0,09 0,02 0,23 0,50 0,55 0,33 0,35 0,53 0,16 MgO 16,31 13,64 28,32 28,92 12,77 28,54 12,25 12,82 12,14 21,49 13,49 13,13 13,02 12,22 CaO 16,04 19,67 0,36 0,28 19,12 0,36 5,11 18,70 5,61 0,03 20,47 4,77 4,70 5,28 5,95 Na 2 O 2,27 2,44 0,05 3,55 0,05 3,24 0,20 0,21 2,33 0,30 0,14 8,65 K 2 O 0,11 0,06 0,01 0,01 0,04 0,04 0,02 9,83 0,02 0,11 100,01 100,00 100,01 100,00 100,01 100,01 100,02 100,00 100,01 100,00 100,01 99,99 99,99 99,99 100,01 Prp 44,8 44,4 47,8 47,6 44,3 Alm 40,8 39,8 39,0 39,4 41,0 Sps 1,0 1,0 0,7 0,7 1,0 Grs 13,3 14,7 12,4 12,3 13,7 Uv 0,1 0,1 0,1 F 18,4 15,6 22,9 21,7 15,0 22,4 47,7 17,1 47,3 14,7 15,7 44,9 45,3 48,1 An, % 28,0 Jd, % 15,3 17,5 20,1 21,9 16,4 Ol (18 20% Fa) (. 2, ) - Opx (En 17 ), - Cpx, Cpx Jd 2,4 8,5% (10%) (. 8,. 2). - - Grt (46 52% Prp, 14 22% Grs) Grt Omp 36 Omp Crn±Pl. -,,.. -. «-» Opx Cpx. Opx (. -32,. 3,. 9) - En 19 Di-Omp 19% Jd Spl. - -,,,, - (. 3,. 3, 4) ( 70 71%, 18 20%, 2,5 4,0%, 7,0 7,5%).,. -30 (. 9), Di 17% Jd - Opx (En 20 ) - - Am, Prg-Hbl, - Cr 2 O 3 (2,11. %), - Di (1,42 2,43. % Cr 2 O 3 ). Omp 20 22% Jd, Grt 47% Prp 15% Grs. (. 3, ) Di 19% Jd, Opx (En 20 ), - Ed-Hbl (3,0. % TiO 2 ) Bt (6,57. % TiO 2 ) Pl (20% An). 47
12 ". 8. "% Ol " 67 %& &$ # $)&$ Opx > ') % & 3 &+ &$ # $)&$ Cpx. \ ( ) $ - #.? * \ $ $ ' ". 9. "% Opx Q# &' % 7 & &) ' (( &- & % 3 &) =6%&/ &$ 7& 5 «' 6 & 50» Q# &' %&. ^ ( ) $ Cpx (19% Jd) Spl. * $ ( ) Opx,, Cpx (17% Jd) Prg-Hbl ( ). ( ) $ Omp (20 22% Jd).? *-32. \ $ $ ' 48
13 Cpx (. 3,. -31) Di 15 17,5% Jd () Opx (En 23 ) - - (. 10, ). -, Omp 20 22% Jd, Grt (44 45% Prp, 13 15% Grs) Opx (En 22 ) Bt (F = 15%, TiO 2 = 3,5. %) (. 10, ). Grt (44 48% Prp, 12 14% Grs) Cpx, - Jd (16%), Pl (28% An) Cpx Grt. - (. 4), - Omp (21 24% Jd), Grt (40 46% Prp, 12 14% Grs), Opx (En ), Am Bt (F = 20 26%, TiO 2 = 4,7 6,2. %). Am Hbl, Act-Hbl, Ed- Hbl Prg-Hbl.,, -, Omp - (. -49) Act-Hbl, Omp, -. Opx -. -, Cpx: Omp Di 18 Di 7-8 ; Am: HblPrg Act-HblPrg-Hbl (. 11,,. 4); - Prp Grt, - Pl (29 34% An) Grt Cpx - (. 11, ) Prg-Hbl Prg Grt+Cpx+H 2 OPl+Prg-Hbl. -., (. 3 11,, ), Omp 2420% Jd - Di 12 Pl 19 Opx (En 33 ). Prp 36%, 35%. - Grt Cpx (Cpx-Pl) Pl (27% An) Bt Am. Fe-Mg F, Bt - TiO 2 (5,5. %) (. 3) -, -, Cpx, Opx. -, Prg-Hbl (. 5,. -171) - Cpx, 12 15% Jd 8% Jd, - (25% An) Cpx - : Di 18 () Opx - 45 ; Grt 15 Omp 20 Opx
14 . 11: -, Cpx (Omp 23 Di 7 ), Am (HblPrg), Grt (Grt 44 Grt 42 ), - Pl ( -33); ( ). -, - (Ed-Hbl Prg-Hbl ), (23% An). - (. 6). 33% Prp 15 16% Grs, 24% Prp 17% Grs.,,, - (Mg-), - (Fe-). -, - --, -., (R-- ) (. 12, ).,,,,,. -, -., - (. 12,, ), - -., -,., -,, -,,, (. 13,, ).,, - (. 12, ). - -., - () -.,,,, -,. -, -, -, -. -, - -, - (. 3) (. 12, ) -,,, 50
15 4 (. -33, -16-3, -49) ( ) Omp Di Grt Bt Opx Omp Hbl Di Act-Hbl Omp Grt Grt Grt Prg Hbl Omp Di Pl Bt SiO 2 54,70 53,13 40,02 39,65 54,38 54,74 51,82 54,04 53,92 54,91 39,62 39,62 39,56 43,96 52,49 54,62 53,18 60,24 39,95 TiO 2 0,10 0,20 0,03 4,67 0,06 1,10 0,18 0,58 0,02 0,02 0,08 1,98 0,89 0,13 0,10 5,24 Al 2 O 3 5,42 3,33 22,12 16,05 1,07 5,67 7,18 5,05 5,50 5,49 22,06 21,98 21,92 14,44 6,73 5,33 2,93 24,61 15,76 Cr 2 O 3 0,43 0,41 0,02 1,80 0,19 0,50 0,28 0,56 0,10 0,89 0,08 0,18 0,10 0,69 0,31 0,52 0,41 0,07 0,77 FeO* 4,45 4,42 20,75 8,55 14,86 4,22 5,99 4,58 6,10 4,33 21,47 21,00 21,32 7,55 6,00 4,46 4,25 0,42 8,81 MnO 0,08 0,55 0,13 0,25 0,08 0,05 0,08 0,02 0,06 0,56 0,57 0,44 0,14 0,02 0,07 0,05 MgO 12,77 15,03 11,84 18,85 28,80 12,44 19,32 13,51 19,99 12,48 11,59 12,06 11,27 15,13 19,32 12,76 15,08 18,91 CaO 18,45 22,28 4,51 0,04 0,33 18,52 12,36 19,38 12,53 18,18 4,59 4,54 5,25 12,65 12,57 18,92 23,01 7,07 0,05 Na 2 O 3,59 1,11 0,15 0,35 0,08 3,73 1,40 2,60 0,91 3,55 2,36 1,26 3,20 0,96 7,41 0,15 K 2 O 0,06 9,89 0,03 0,47 0,36 0,05 0,02 0,02 1,11 0,40 0,04 0,01 0,11 10,36 Sum 99,99 99,97 99,99 99,98 99,96 99,99 99,97 99,98 100,01 99,96 99,97 99,99 99,96 100,01 99,97 100,00 100,00 99,98 100,00 Prp 43,9 42,5 43,7 41,5 Alm 42,9 44,1 42,9 43,7 Sps 1,3 1,3 1,3 1,0 Grs 11,9 12,0 12,0 13,7 Uv 0,1 0,1 0,1 F 16,3 14,2 49,4 20,3 22,4 16,0 14,8 16,0 14,6 16,3 50,9 49,4 51,3 21,9 14,8 16,4 13,7 20,7 An, % 34,3 Jd, % 23,0 8,1 24,1 18,2 23,4 22,6 6, Grt Omp Opx Di Ed-Hbl Grt Grt Pl Act-Hbl Act-Hbl Prg-Hbl Bt Bt Opx Opx Grt Grt Omp Omp Pl Di Opx Bt Pl SiO 2 41,08 53,60 53,68 51,53 43,08 39,78 39,52 60,99 52,83 53,37 44,21 39,40 39,45 54,79 54,56 38,63 38,84 52,91 52,02 63,16 53,05 53,70 38,73 61,23 TiO 2 0,04 0,04 0,14 1,93 0,48 0,49 1,23 5,72 6,24 0,05 0,11 0,08 0,14 0,38 0,01 0,24 5,47 0,05 Al 2 O 3 22,47 6,06 0,58 4,36 13,24 22,47 22,31 24,12 6,12 5,52 13,99 15,22 15,64 0,50 0,76 22,06 21,89 7,08 6,76 22,75 3,61 0,77 15,75 23,78 Cr 2 O 3 0,03 0,67 0,82 0,66 0,01 0,25 0,02 0,24 0,27 0,53 0,28 0,47 0,04 0,06 0,07 0,14 0,23 0,03 0,41 FeO* 18,68 4,47 15,46 4,38 8,50 20,34 21,08 0,36 7,39 7,53 9,95 10,75 10,97 15,76 17,26 23,59 22,82 6,68 6,34 0,17 6,27 20,76 12,65 0,23 MnO 0,36 0,04 0,18 0,44 0,64 0,01 0,04 0,22 0,13 0,69 0,57 0,18 0,09 0,08 0,07 0,18 0,12 MgO 12,28 12,51 29,69 13,96 15,99 12,07 10,74 19,40 19,51 14,09 18,41 17,38 28,03 26,98 9,51 9,91 11,87 11,77 13,32 24,00 16,16 0,01 CaO 4,99 18,83 0,39 23,50 12,26 4,88 5,46 6,18 11,49 11,48 12,19 0,03 0,27 0,24 5,34 5,72 17,73 19,68 4,09 21,51 0,38 0,12 5,79 Na 2 O 0,06 3,77 1,30 2,75 8,22 1,64 1,45 2,55 0,31 0,19 0,32 0,08 0,03 3,37 2,76 9,34 1,69 0,13 0,02 8,60 K 2 O 0,03 0,08 0,95 0,02 0,01 0,11 0,41 0,38 1,23 9,88 9,66 0,02 0,05 0,28 10,41 0,15 Sum 100,02 99,99 100,06 99,99 99,36 100,01 100,01 100,00 100,01 100,00 100,01 100,00 100,00 100,00 99,99 100,01 99,98 99,96 99,94 99,88 99,99 99,95 99,72 99,96 Prp 46,4 44,4 40,1 35,3 36,4 Alm 39,3 41,8 44,1 49,0 47,0 Sps 0,7 1,0 1,3 1,3 1,3 Grs 13,6 12,8 14,4 14,4 15,2 Uv 0,1 0,1 F 45,9 16,7 22,6 15,0 23,0 48,5 52,4 17,6 17,8 28,4 24,7 26,1 24,0 26,4 58,1 56,4 24,0 23,3 20,9 32,7 30,5 An, % 29,2 19,2 26,9 Jd, % 20,9 8,8 23,7 19,5 12,00 -- (14% An), (. 12, ), - Pl+Qtz Pl >Na +Ky (, 1990) (. 5,. -171), - (. 5,. -171)., -, - (. 13, ). (27% Prp, 20 23% Grs) - (F = 39%), (F = 35%, TiO 2 = 4,01. %) (20 24% An). 4% Jd. (. 13, ), (F = 38%), (F = 31%, TiO 2 = 3,2. %), (22 25% An) 7 10% Jd., -,, -. 51
16 5 - (. -171) (. -171) Di Prg-Hbl Pl Di Di Prg-Hbl Grt Grt Pl Prg-Hbl Ed-Hbl Prg-Hbl Grt SiO 2 51,32 44,61 62,17 50,18 50,77 44,07 38,81 39,10 63,33 44,42 45,50 44,22 37,28 TiO 2 0,08 1,46 0,01 0,23 0,12 1,75 0,21 0,14 1,16 1,23 1,68 0,01 Al 2 O 3 7,60 12,12 23,28 6,66 6,63 12,31 21,74 21,89 22,79 12,18 11,18 11,98 21,35 Cr 2 O 3 0,25 0,44 0,06 0,14 0,20 0,38 0,08 0,03 0,02 0,03 0,12 0,01 FeO* 7,12 12,59 0,21 7,48 7,05 13,21 23,95 23,62 0,11 14,01 13,72 14,13 27,59 MnO 0,20 0,02 0,02 0,17 0,17 0,16 0,65 0,83 0,08 0,14 0,08 0,85 MgO 11,26 12,92 0,01 12,12 11,61 12,53 8,89 8,65 12,96 13,38 12,81 6,46 CaO 19,99 12,49 5,30 21,83 21,73 12,43 5,61 5,84 4,73 12,32 12,21 12,50 6,42 Na 2 O 2,13 1,83 8,66 1,11 1,68 1,72 0,06 8,69 1,61 1,59 1,52 K 2 O 0,05 1,33 0,25 0,05 0,04 1,27 0,18 1,13 0,86 1,03 100,00 99,81 99,97 99,97 100,00 99,83 100,00 99,96 99,99 99,9 99,93 99,95 99,97 Prp 33,2 32,7 23,9 Alm 50,3 49,8 57,0 Sps 1,3 1,7 1,9 Grs 15,1 15,8 17,2 Uv 0,1 F 26,2 35,3 25,7 25,4 37,2 60,2 60,4 37,8 36,5 38,2 70,5 An, % 24,9 22,9 Jd, % 15,4 8,2 12, Grt Grt Pl Ed-Hbl Di Pl Bt Pl Grt Grt Bt Pl Di Di Prg-Hbl Pl SiO 2 38,54 37,89 61,47 45,05 53,01 63,12 39,50 63,07 39,24 38,50 38,55 62,91 51,03 50,63 43,98 61,91 TiO 2 0,13 0,04 1,37 0,24 0,03 4,01 0,03 0,07 0,08 3,23 0,34 0,32 1,50 0,10 Al 2 O 3 21,67 21,74 23,41 12,17 1,71 22,74 15,28 22,93 22,07 21,77 15,58 23,39 5,36 6,71 13,17 23,52 Cr 2 O 3 0,08 0,14 0,06 0,05 0,11 0,01 0,07 0,12 0,04 0,05 0,09 0,01 FeO* 22,96 24,34 0,39 14,01 6,80 0,16 14,83 0,11 22,64 23,35 12,93 0,13 8,03 7,88 13,59 0,21 MnO 0,61 1,04 0,03 0,18 0,08 0,02 0,60 0,62 0,01 0,07 0,05 0,07 0,05 MgO 7,24 7,16 0,06 12,19 14,24 0,05 15,78 7,03 6,94 16,13 0,01 12,01 11,73 12,32 0,02 CaO 8,66 7,47 5,28 12,55 23,12 4,28 0,02 4,68 8,26 8,65 0,07 4,53 22,11 21,18 11,92 5,29 Na 2 O 0,10 0,13 8,78 1,36 0,62 9,24 8,79 0,07 2,16 8,58 1,01 1,39 1,88 8,52 K 2 O 0,05 0,40 1,22 0,21 10,34 0,38 9,67 0,39 1,35 0,34 99,99 100,0 99,88 99,92 99,92 99,96 99,89 100,0 99,98 99,98 98,44 99,99 99,96 99,94 99,87 99,97 Prp 27,2 26,6 27,2 26,2 Alm 48,2 51,0 48,7 49,2 Sps 1,3 2,3 1,3 1,3 Grs 23,2 20,0 22,8 23,2 Uv 0,1 0,1 0,1 F 63,9 65,7 39,2 21,1 34,5 64,2 65,2 31,0 27,3 27,3 38,2 An, % 24,4 20,1 22,2 22,1 25,1 Jd, % 4,4 7,3 9,9 6 (I ) (. -35, -53) Grt Grt Di Pl Di Di Pl Ed Omp Ed-Hbl Prg-Hbl Pl SiO 2 37,48 38,01 50,51 62,79 50,30 50,07 62,88 46,61 50,93 44,43 43,11 62,52 TiO 2 0,26 0,04 0,26 0,36 0,42 1,18 0,20 1,06 0,97 0,02 Al 2 O 3 20,80 21,25 4,82 22,61 4,01 4,14 22,51 9,69 8,63 11,48 12,57 23,14 Cr 2 O 3 0,02 0,18 0,10 0,05 0,03 0,10 0,08 0,09 FeO* 26,86 25,26 10,66 0,18 9,74 10,38 0,11 15,60 9,14 16,44 16,66 0,13 MnO 0,67 0,45 0,15 0,06 0,07 0,07 0,12 0,12 MgO 5,66 5,94 12,02 0,01 11,55 11,89 11,18 9,13 11,42 11,07 CaO 8,17 9,00 20,29 4,76 22,79 21,84 4,56 13,22 18,67 12,45 12,55 4,92 Na 2 O 0,99 9,19 1,13 1,07 9,60 1,55 3,12 1,78 1,75 8,82 K 2 O 0,09 0,30 0,14 0,28 0,65 0,76 0,90 0,32 99,92 99,95 99,97 100,00 100,00 99,98 99,94 99,85 99,94 99,82 99,78 99,96 Prp 21,1 22,2 Alm 55,9 52,6 Sps 1,3 1,0 Grs 21,7 24,2 Uv F 72,6 70,4 33,3 32,2 32,9 43,9 35,9 44,7 45,8 An, % 21,9 20,5 23,1 Jd, % 7,6 8,2 8,4 22,3 52
17 Omp Omp Omp Di + Pl Omp Di + Pl Grt Grt Grt + Omp Omp + Grt SiO 2 52,46 52,17 51,73 50,70 62,96 52,12 50,04 63,23 37,86 38,06 37,88 51,41 51,47 38,18 TiO 2 0,20 0,17 0,43 0,28 0,30 0,32 0,01 0,07 0,14 0,49 0,31 0,08 Al 2 O 3 9,19 9,30 8,59 4,87 22,82 8,03 6,85 22,86 21,28 21,21 21,23 7,35 8,44 21,32 Cr 2 O 3 0,05 0,04 0,02 0,01 0,04 0,01 0,09 0,03 0,13 0,08 FeO* 8,69 8,68 8,78 10,24 0,20 9,51 10,89 0,28 26,01 24,87 25,20 8,55 8,71 25,43 MnO 0,16 0,06 0,16 0,17 0,02 0,10 0,02 0,61 0,58 0,56 0,02 0,01 0,36 MgO 8,55 8,55 8,83 11,05 9,01 10,22 5,71 6,36 6,17 9,90 9,35 5,83 CaO 16,10 16,35 17,13 20,98 4,17 17,06 19,32 4,12 8,42 8,78 8,93 18,47 17,79 8,80 Na 2 O 4,61 4,69 4,32 1,63 9,37 3,97 2,16 9,15 3,68 3,85 K 2 O 0,07 0,42 0,02 0,32 0,04 100,01 100,01 99,99 100,00 100,00 100,01 100,01 99,99 100,00 100,00 100,00 100,01 100,01 99,99 Prp 21,4 23,5 22,8 21,8 Alm 54,6 51,7 52,2 53,7 Sps 1,3 1,3 1,3 0,7 Grs 22,7 23,5 23,7 23,8 Uv F 36,4 36,3 35,8 34,3 37,2 37,4 71,9 68,8 69,7 32,7 34,3 71,1 An, % 19,3 19,6 Jd, % 32,5 33,1 30,6 12,1 28,2 15,6 26,1 27, : (. 1-, ); Pl - Cpx Bt ( ); Grt-Cpx-Am-Bt (., 179-1,.. 3); Pl Ky (., )
18 . 13. Grt-Cpx-Am-Bt -, (.. 3). -, -, - (,, -,.), -, - - -, -, ,,,,. - (F = 18 20%) - -, -,,. -- (Jackson, 1969) (. 2) 930 C (. 7), -. (. 2,. 21, 22) Al 2 O 3 (1,03 2,72. %) CaO (2,36 2,39. %) (En ) (, 1981; -, 2000;., 2004). - (. 9),,,,, -, -, - (En 19 ) Cpx (Di-Omp 19 ) - (Di 17 ) Opx (En) Prg-Hbl.,,, (En ), (En ) (Di); - (En ), - (En ) - (En 33 ). - Opx - Al 2 O 3 CaO. -,, - (- ), - Na 2 O. 7 -,,. Ol-Spl Opx-Cpx Jd Ol F Spl Opx F Cpx Jd (1) (2) (3) Ol 20 Spl En 19 DI , En 23 Di , En 19 Di ,0. : (1) Jackson, 1969; (2) Brey, Kohler, 1990; : (3) Holland,
19 . 14 Jd--, -,,. - - (., 2004). - - (. 10),, - (. 5). ( - ) 9 14% 19% Jd. Opx-Cpx - - (En 19 Di 12,. 5) - (En 23 Di 18,. 10 En 19 Di 19,. 9) - (Brey, Kohler, 1990) - Jd (Holland, 1980) - (. 7,. 15), - Opx Cpx () «-» (Grt 47 Omp En 20 ) (Grt 44 Omp En 22 ) (. 8,. 15) C - - (. 15). - - Fe-Mg,,,,,, - (12 17%) (. 16).., - Jd (9 11%) - Cpx,, - Jd (., 2004), -, ( 18, 20, 27 Grt Omp 21-22,. 8,. 15). - Cpx Jd %, - Opx Cpx (28 41% Jd), (Grt ),, (Grt 48 Omp 30-38,. 7, ), - Omp Grt ± Omp 46 Omp Crn Omp Crn+Pl (. 6, ) Omp Grt 45 + Omp 57 +Crn Omp 37 +Crn+Pl 15 (. 6, ) C (. 8) Cpx
20 : 1, 2 (?) ; 3 8 (3) - : Omp Crn+Pl (4), Grt Di±Pl, Qtz (5), Am Pl-Qtz±Grt (6) (7), Di Am - (8); 9 13 : (I - ) (9) Grt Di Pl Qtz (10) Am Pl Qtz (11) - ; Grt Di Pl Qtz, Di Am (12) Grt Am Pl Qtz (13); (14) (I ) (15). Jd Cpx : Holland, 1980; Ky Sil : Holland, Powell, 1990; Gln : Maresh, 1977; (), () () : Cloos, Si,,.. (2005),, Ab = Jd+Qtz, Ne+Ab = Jd, - (Harlow, 1994). Omp Crn Omp Crn+Pl 15-18, Omp Ab. Omp Crn+Pl 15-18,, - Omp Omp Pl ( ) C 14 9 (. 8,. 15) = C, = 11,7 8,5. - ( = C, = 11,0 6,7 ), - ( = C, = 9,0 6,9 ) ( , , 37, 39,. 8,. 15). -. -,, -, , (. 1) ( I), - -,, - -- ( II)., - 56
21 Fe ( = 930 C, = 17,5,. 8) - Cpx-Pl, Cpx Omp Di 8 (. 6), - -, - ( = C, = 7,3 7,5 ) / -30/1-30/2-30/3.,, - Grt-Cpx Cpx-Hbl Hbl-Pl-Qtz Grt-Hbl Jd Grt-Cpx-Pl-Qtz Hbl Grt Prp Cpx Jd Pl An Am (1) (2) (3) (4) (5) (6) (7) 5 Grt 49 Omp ,2 6 Grt 49 Omp ,5 7 Grt 49 Omp ,5 8 Grt 48 Omp ,6 9 Grt 48 Omp ,8 10 Grt 51 Omp ,0 11 Grt 50 Omp ,0 12 Grt 48 Omp ,2 13 Grt 48 Omp ,2 14 Grt 45 Omp , Grt 52 Omp ,5-30/4 16 Grt 49 Di-Omp ,5-31/2 17 Grt 45 Omp ,4-31/3 18 Grt 44 Omp ,7-31/4 19 Grt 48 Di ,4 20 Grt 47 Omp , Grt 47 Omp-Di ,8-33/1 22 Grt 44 Omp ,9 23 Grt 44 Omp ,8 24 Grt 43 Di ,7-33/2 25 Grt 42 Di 7 Pl ,5 26 Grt 43 Pl 34 Prg , Grt 46 Omp , Pl 30 Prg-Hbl 705 8,3-16/ Grt 37 Omp Grt 35 Omp c 31 Grt 35 Di 7 Pl ,3 32 Di 12 Prg-Hbl ,0 33 Pl 25 Prg-Hbl ,0 34 Grt 33 Pl 23 Prg-Hbl ,8 35 Grt 24 Pl 23 Prg-Hbl ,7 36 Grt 27 Pl 24 Ed-Hbl ,9 37 Grt 27 Di 4 Pl ,0 38 Di 10 Prg-Hbl ,5 39 Grt 27 Pl 25 Prg-Hbl ,7 40 Grt 24 Omp ,5 41 Grt 24 Omp ,1 42 Grt 24 Omp ,3 43 Grt 23 Di 16 Pl ,3 13,3 44 Grt 23 Prg-Hbl 650 7,5 45 Grt 22 Omp ,2 46 Grt 21 Di 8 c Pl ,9 47 Pl 23 Prg-Hbl 700 7,3. : (1) Powell, 1985; (2), 1986; (3) Holland, Blundy, 1994; (4),, 1989; : (5) Holland, 1980; (6) Perkins, Newton, 1981; (7) Blundy, Holland, ,
22 - -, -,, , - (., 2005) Grt - (1 5) (1), - (2) (3), (4) (5) - (6 7) - (6) (7) Fe-Mg - (. 6). (. 16) Grt-Cpx. - -.,, - - 2,7, 2,45 2,40 1,9 1,8 (, 1990), -,,... ( = C, = 14,0 17,5 ) 2720±8 (., 2003;., 2004), -. -.,, (Slabunov, Stepanov, 1998), -. 2,7 (., 2004) -, - - ( = C, = 14,0 13,0 6,5 ).,, ,, -, - (), , -., (-, 1981), 2416,3±1 (., 2003). -,, (1,9 1,8 ), -.,,,, -. -, - - (, 1990) ). --,, -,,, - ( ) -. 2) - 58
23 - -, -,, - -, - -. II - - (. 2, ) (II ), - = 6,7 7,7 = C, , -,, , -. - ( ) -. -, - - = 900 C 700 C = C -., -, - Jd Omp 33 36% ( = 15, = C),,., ( 20 ) ( 930 C) Jd Omp 57%,,, -, , -,, () -, -. ( = 0, = 0),. -, -, - - -, -, -, - - (..., 2004) (),.... ( ) -...,.., ( ) //. II -.., , ,..,... - (- ) // , ,.., ( 59
24 ) // :,,,.... -, ,..,.. - : // , //.. XXIII...., , ,.. ( ): U-Pb Sm-Nd // - :,,,.... -, , - // ,.. - ( ) // , (- ) -, // , , //.., ,.., //.. 3., ,..,.. U-Pb, Nd - ( ) // II.. «-».., , ,.. :,, // - :,, -,... -., ,..,... (2.1. ) Fe- - : -, // , , ,.., () // , ,..,... -,,, :, - - // - :,, -,...., Blundy J. D., Holland T. J. B. Calcic amphibole equilibria and a new amphibole-plagioclase geothermometer // Contrib. to Mineral. and Petrol Vol. 104, N 2. P Brey G. P., Kohler T. Geothermobarometry in four-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometer // J. Petrol Vol. 31, N 6. P Cawthorn R. G., Collerson K. D. The recalculation of pyroxene end-member parameters and the estimation of ferrous and ferric iron content from electron microprobe analyses // Amer. Mineral Vol. 59, N P Cebria J. M. PX: A program for pyroxene classification and calculation of end-members // Amer. Mineral Vol. 75. P Chopin C. Ultrahigh-pressure metamorphism: tracing continental crust into the mantle // Earth and Planet. Sci. Letters P Cloos M. Litospheric buoyancy and collisional orogenesis: subduction of oceanic plateaus, continental margins, island areas, spreading ridges and seamounts // Geol. Soc. Amer. Bull Vol. 105, N 6. P Eskola P. On the eclogites of Norway. Skr. Vidensk. Selsk. Christiania. Mat.-Nat K P Godard G. Eclogites and their geodynamic interpretation: a history // Journal of Geodynamics N 32. P Griffin W. L. «On the eclogites of Norway» 65 years later // Mineralogical Magazine Vol. 51, N 361. P Harlow G. E. Jadeitites, albitites and related rocks from the Motagua Fault Zone, Guatemala // Jour. Metam. Geol Vol. 12. P Holland T. J. B. The reaction albite=jadeite+quartz determined experimentally in the range grad. C // Amer. Mineral Vol. 65. P Holland T. J. B., Blundy J. D. Non-ideal interactions in calcic amphiboles and their bearing on amphibole-plagioclase thermometry // Contrib. to Mineral. and Petrol Vol P Holland T. J. B., Powell R. An enlarged and updated internally consistent thermodynamic dataset with uncertainties and corrections: the system K 2 O-Na 2 O-CaO-MgO-MnO-FeO- Fe 2 O 3 -Al 2 O 3 -TiO 2 -SiO 2 -C-H 2 -O 2 // J. Metamorphic Geol Vol. 8. P Jackson E. D. Chemical variation in coexisting chromite and olivine in chromitite zones of the Stillwater complex // Economic Geology Vol. 4. P John T., Schenk V. Partial eclogitization of gabbroic rocks in a late Precambrian subduction zone (Zambia): prograde metamorphism triggered by fluid infiltration // Contrib. to Mineral. and Petrol Vol P Koons P. O., Rubie D. C., Frueh-Green G. The effects of disequilibrium and deformation on the mineralogical evolution of quartz-diorite during metamorphism in the eclogite facies // Journal of Petrology P Lappin M. A., Smith D. C. Mantle-equilibrated eclogite pods from the basal gneisses in the Selje district, Western Norway // Journal of Petrology N 19. P Leak B. E. Nomenclature of amphiboles // Amer. Mineral Vol. 63, N P
25 Lobach-Zhuchenko S. B., Arestova N. A., Chekulaev V. P. et al. Geochemistry and petrology of Ga magmatic rocks in the north-western Belomorian Belt, Fennoscandian Shield, Russia // Precambrian Research Vol Maresh W.V. Experimental studies on glaucophane: an analysis of present knowledge // Tectonoph Vol. 43. P Morimoto N. Nomenclature of pyroxene // Mineral. Mag Vol. 52, N 4. P Mørk M. B. Coronite and eclogite formation in olivine gabbro (Western Norway): reaction paths and garnet zoning // Mineralogical Magazine P Perkins D.III, Newton R.C. Charnockite geobarometers based on coexisting garnet-pyroxene-plagioclase-quartz // Nature Vol. 292, N 9. P Pognante U. Coronitic reactions and ductile shear zones in eclogitized ophiolite metagabbro, Western Alps, north Jtaly // Chemical Geology P Powell R. Regression diagnostics and robust regression in geothermometer/geobarometer calibration: the garnetclinopyroxene geothermometer revised // J. Metamorph. Geol Vol. 3, N 3. P Slabunov A. I., Stepanov V. S. Late Archean ophiolites of the Belomorian Mobile Belt, Fennoscandian/Baltic Shield: why not? // International Ophiolite Symposium and Field Excursion. Generation and Emplacement of Ophiolites through time, August Oulu, Finland. Geol. Survey of Finland, Special Paper 26. P. 56. Wayte G. J., Worden R. H., Rubie R. C. et al. A TEM study of disequilibrium plagioclase breakdown at high pressure: the role of the infiltrating fluid // Contrib. to Mineral. and Petrol Vol P
REE-mineralogy of Suhuvaara appinite, Inari, Northern Finland Thair Al-Ani and Olli Sarapää
Northern Finland Unit M42/2010/67 22.2.2011 Rovaniemi REE-mineralogy of Suhuvaara appinite, Inari, Northern Finland Thair Al-Ani and Olli Sarapää GEOLOGICAL SURVEY OF FINLAND DOCUMENTATION PAGE Date /
More informationThe plagioclase, forsterite, diopside, liquid equilibrium in the system
MINERALOGICAL MAGAZINE, SEPTEMBER 1981, VOL. 44, PP. 309-14 The plagioclase, forsterite, diopside, liquid equilibrium in the system CaO-Na20-MgO-AI203-SiO 2 G. M. BIGGAR AND D. J. HUMPHRIES Department
More informationThe application of multidimensional wavelets to unveiling multi-phase diagrams and in situ physical properties of rocks
Earth and Planetary Science Letters 223 (2004) 49 64 www.elsevier.com/locate/epsl The application of multidimensional wavelets to unveiling multi-phase diagrams and in situ physical properties of rocks
More informationDownloaded from ijcm.ir at 14: on Friday January 25th 2019 ! "#$% & ' ' ( )* !4/54.
Downloaded from ijcm.ir at 14:3 +0330 on Frida Januar 5th 019 I wx4>!- _- 6" 7 &' _ $%! " 0/ *. $ / 0 1'( / 0 ( / / * +,! - & ' ' ( )* "., - &'() "*+, : / / :! "$% ) /-*= @ / 0= $ 6$0 '=(?9 6 (=>
More informationDATA REPOSITORY. G. Di Vincenzo, A. Grande, F. Rossetti CONTENTS
DATA REPOSITORY Paleozoic siliciclastic rocks from northern Victoria Land (Antarctica): provenance, timing of deformation and implications for the Antarctica/Australia connection G. Di Vincenzo, A. Grande,
More informationCSpace: an integrated workplace for the graphical and algebraic analysis of phase assemblages on 32-bit wintel platforms p
Computers & Geosciences 26 (2000) 779±793 CSpace: an integrated workplace for the graphical and algebraic analysis of phase assemblages on 32-bit wintel platforms p Rafael L. Torres-Roldan a, *, Antonio
More informationProgram Gibbs. Tutorial. Frank S. Spear by Frank S. Spear
Program Gibbs Tutorial by Frank S. Spear 2001 by Frank S. Spear F. S. Spear Program Gibbs Tutorial 2 Program Gibbs Tutorial February, 2001 Frank S. Spear Department of Geology, Rensselaer Polytechnic Institute,
More informationMeet with your Advisor every semester!!"
for Spring 2016 Meet with your Advisor every semester! If you don t know who your advisor is # Your primary advisor s name is listed in DegreeWorks in the top row and it should also appear in Banner under
More informationGEOPT19 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES REPORT ON ROUND 19 / July 2006 (Gabbro, MGR-N)
GEOPT19 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES REPORT ON ROUND 19 / July 2006 (Gabbro, MGR-N) Peter C. Webb 1 *, Michael Thompson 2, Philip J. Potts 1 and B. Batjargal
More informationBMR GEOLOGY AND GEOPHYSICS AUSTRALIA MINERAL DATA ANALYSIS SYSTEM (MDA) REFERENCE MANUAL. Record 1992/3. BMR PUi;Lh.":h.~ - (LENDING S):.,L.l.1...,.
BMR GEOLOGY AND GEOPHYSICS AUSTRALIA I MINERAL DATA ANALYSIS SYSTEM (MDA) REFERENCE MANUAL Record 1992/3 BMR PUi;Lh.":h.~ - (LENDING S):.,L.l.1...,." J J J J J J +..... ~. ~. by AL Jaques, L Simons and
More informationCourse Syllabus. Optical Mineralogy. Course Name:
The University of Jordan Accreditation & Quality Assurance Center Course Syllabus Course Name: Optical Mineralogy 1 Course title Optical Mineralogy 2 Course number 0305211 Credit hours (theory, practical)
More informationGEMS Tutorial, A. Gysi, D. Kulik and D. Miron August 2018
MODULE 1: CREATING YOUR FIRST PROJECT IN GEMS AND INSTALLING THE MINES DATABASE GEM-Selektor (GEMS), is a numerical modeling program with a graphical user interface based on Gibbs energy minimization and
More informationalphamelts, libalphamelts and libphmelts; application to LLD
alphamelts, libalphamelts and libphmelts; application to LLD MELTS Short course, Goldschmidt, June, 2016 Paula Antoshechkina, Paul Asimow & Mark Ghiorso. psmith@gps.caltech.edu asimow@gps.caltech.edu ghiorso@ofm-research.org
More informationCompute the chemical equilibria of single chemical systems (SysEq)
MODULE 2: REACTION PATH MODELING In this tutorial, you will learn to model the reaction path of K-feldspar in contact with a NaCl-bearing aqueous solution and calculate the evolution of the fluid and the
More informationPerplex Tutorial I: Installation and a simple ternary diagram!
D. Hirsch, 1/2014 Perplex Tutorials Perplex Tutorial I: Installation and a simple ternary diagram Basics Perplex is a collection of programs, each designed to accomplish a different task. These are command-line
More informationU.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Analytical Data-Management Systems: 2. Normalization, Atomicity, and Structure of Geosciences Data by J.T. O'Connor 1 Open-File Report 94-406 This
More informationSiemens Safety Integrated Take a safe step into the future
Engineered with TIA Portal Machine Safety Life-Cycle Siemens Safety Integrated Take a safe step into the future Unrestricted / Siemens Industry Inc. 2015. All Rights Reserved. www.usa.siemens.com/safety
More informationLA ICP MS Analysis with
LA ICP MS Analysis with V 1.0.4 04.06.2008 Software written by Murray Allan at Die Eidgenössische Technische Hochschule Zürich, CH and the University of Leeds, UK Additional Software writing: Dimitri Meier
More informationGeoPT22 - MBL-1, Basalt
GeoPT22 - MBL-1, Basalt Veranstalter: International Association of Geoanalysts and Geostandards Newsletter - GeoPT22 Ringversuchsmaterial: MBL-1, Basalt RV geschlossen: 2008 2 Literatur: Proficiency Testing
More informationGeodynamic models 20 years past and future
www.sci.monash.edu Geodynamic models 20 years past and future Louis Moresi, School of Earth Sciences, University of Melbourne 1994 1999 2004 2009 2014 1 Plate tectonics a multi-scale problem 2 Integrated
More informationALPHAMELTS SOFTWARE MANUAL.
ALPHAMELTS SOFTWARE MANUAL. A text driven interface for MELTS, pmelts & phmelts. Paula Antoshechkina (psmith@gps.caltech.edu) & Paul Asimow (asimow@gps.caltech.edu). October 13, 2017 (Version 1.8). ABSTRACT
More informationAN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES REPORT ON ROUND
GeoPT23 AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES REPORT ON ROUND 23 (Separation Lake pegmatite, OU-9) and 23A (Manganese nodule, FeMn-1) / August 2008 Peter C. Webb 1
More informationOptical Mineralogy in a Nutshell
Optical Mineralogy in a Nutshell Use of the petrographic microscope in three easy lessons Courtesy of Jane Selverstone University of New Mexico Part I Why use the microscope?? Identify minerals (no guessing!)
More informationDownloaded from ijcm.ir at 1: on Sunday April 29th 2018 ? +,( 7FD1 DF 7FD1?&4P? " 4E
' ( ( E 3 D. 3 *+ 4 + E NPZ >* 23,* "1- F C 5 III II % &. 0 " - 5 # " 6 * 3401 "+2 * *# * -#. +, # %& ' (* ( : : # "!! " #.+9 GF2 E * '*4% A#B C D. 695 +, @#. * III II ;+
More informationMGDS Data Exploration Tools Hands-on exercises and usability feedback
MGDS Data Exploration Tools Hands-on exercises and usability feedback Please try the following short exercises. Remember, there are multimedia tutorials and help pages at this web page: http://www.geomapapp.org/
More informationEarth Science. 1 st Nine Weeks problems 22-28% Strand
Earth Science The Earth Major geologic events that occur over eons or brief moments in time continually shape and reshape the surface of the Earth, resulting in continuous global change. 1 st Nine Weeks
More informationGEOPT10 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES - REPORT ON ROUND 10 / December 2001 (CH-1 marine sediment).
GEOPT10 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES - REPORT ON ROUND 10 / December 2001 (CH-1 marine sediment). Philip J. Potts 1 *, Michael Thompson 2, Peter C. Webb
More informationSeismic refraction surveys
Seismic refraction surveys Seismic refraction surveys generate seismic waves that are refracted back to Earth s surface from velocity and density discontinuities at depth. Uses : Small-scale: geotechnical
More informationThe View Data module
The module Use to examine stored compound data (C p (T),H, G, S, etc.) in Compound databases and list solution phases in Solution databases. Table of contents Section 1 Section 2 Section 3 Section 4 Section
More informationRHM160. Coriolis Mass Flow Meter for High Flow Terminal and Pipeline Applications. Features. Applications. Benefits
RHM160 Coriolis Mass Flow Meter for High Flow Terminal and Pipeline Applications Features Standard Pressure ratings up to 50bar (725 psi) Temperature ratings from -196 to 120 C (-320 to 248 F) Mass flow
More informationSo il Geochem ica l Ba seline and Env ironm en ta l Background Va lues of Agr icultura l Reg ion s in Zhejiang Prov ince.
2007, 23 (2) : 81-88 Journal of Ecology and Rural Environm ent 1, 1, 2, 1 (1., 311203;, 065000) 2. :,, 13,,, 52(), : ; ; ; : P632; X8; P59 : A: 1673-4831 (2007) 02-0081 - 08 So il Geochem ica l Ba seline
More informationACTIVE FLOW CONTROL IN TWIN AIR-INTAKE USING VORTEX GENERATORS JETS
Proceedings of the International Conference on Mechanical Engineering 11 (ICME11) 18- December 11, Dhaka, Bangladesh ICME11-FL-24 ACTIVE FLOW CONTROL IN TWIN AIR-INTAKE USING VORTEX GENERATORS JETS Akshoy
More informationGEOPT13 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES - REPORT ON ROUND 13 / July 2003 (Köln Loess)
GEOPT13 - AN INTERNATIONAL PROFICIENCY TEST FOR ANALYTICAL GEOCHEMISTRY LABORATORIES - REPORT ON ROUND 13 / July 2003 (Köln Loess) Philip J. Potts 1 *, Michael Thompson 2, Simon R.N. Chenery 3, Peter C.
More informationReservoir Modeling Combining Geostatistics with Markov Chain Monte Carlo Inversion
Reservoir Modeling Combining Geostatistics with Markov Chain Monte Carlo Inversion Andrea Zunino, Katrine Lange, Yulia Melnikova, Thomas Mejer Hansen and Klaus Mosegaard 1 Introduction Reservoir modeling
More informationTh C 02 Model-Based Surface Wave Analysis and Attenuation
Th C 02 Model-Based Surface Wave Analysis and Attenuation J. Bai* (Paradigm Geophysical), O. Yilmaz (Paradigm Geophysical) Summary Surface waves can significantly degrade overall data quality in seismic
More informationSpecial Documentation Proline Promag 400 HART
SD01847D/06/EN/01.16 71340791 Valid as of version 02.00.zz (Device firmware) Products Solutions Services Special Documentation Proline Promag 400 HART Heartbeat Verification + Monitoring application package
More informationSample Introduction Systems SOLID LASER ABLATION -II
Sample Introduction Systems SOLID LASER ABLATION -II Analyte 193 nm system Frames Cell The FRAME defines the gas volume, mixing and flow dynamics of the chamber as seen with the teardrop frame. The sample
More informationComparison between Neighbourhood and Genetic Algorithms on two Analytic Objective Functions and on a 2.5D Synthetic Seismic Inverse Problems
Comparison between Neighbourhood and Genetic Algorithms on two Analytic Objective Functions and on a 2.5D Synthetic Seismic Inverse Problems A. Sajeva*, M. Aleardi*, A. Mazzotti* and E. Stucchi** * Università
More informationRobust Design Methodology of Topologically optimized components under the effect of uncertainties
Robust Design Methodology of Topologically optimized components under the effect of uncertainties Joshua Amrith Raj and Arshad Javed Department of Mechanical Engineering, BITS-Pilani Hyderabad Campus,
More informationA Really Good Log Interpretation Program Designed to Honour Core
A Really Good Log Interpretation Program Designed to Honour Core Robert V. Everett & James R. Everett CWLS Summary: Montney example illustrates methodology We have unique, focussed, log interpretation
More informationVolume 5, Issue 7, July 2017 International Journal of Advance Research in Computer Science and Management Studies
Volume, Issue 7, July 2017 International Journal of Advance Research in Computer Science and Management Studies Research Article / Survey Paper / Case Study Available online at: www.ijarcsms.com A Study
More informationMicro-CT in geosciences: Getting the inside story. Wesley De Boever
Micro-CT in geosciences: Getting the inside story Wesley De Boever November 24, 2016 Bruker microct Micro-CT scanner manufacturer Life science and material science Hardware and software Headquarters in
More informationSpace Groups. Space Groups. Space Groups: Learning Goals. Space Groups. Lattices (centering operations) Space Groups: Learning Goals 9/18/2017
Space Groups Space Groups Internal Symmetry of Crystals Dyar, Gunter, Tasa chapt 12 If translation operations are included with rotation and inversion, We have 230 three-dimensional space groups. Translation
More informationGuidelines for Spectral Library Generation, Documentation, Dissemination, and Archiving. PDS Geosciences Node Washington University in St.
Guidelines for Spectral Library Generation, Documentation, Dissemination, and Archiving PDS Geosciences Node Washington University in St. Louis CRISM Spectral Library Working Group Input from Mars Spectroscopy
More informationThe evolution of the cookbook
The evolution of the cookbook Angela E. Summers, Ph.D., P.E Michela Gentile, Ph.D. Mary Kay O Connor Process Safety Center 2006 International Symposium Beyond Regulatory Compliance, Making Safety Second
More informationApplication of MPS Simulation with Multiple Training Image (MultiTI-MPS) to the Red Dog Deposit
Application of MPS Simulation with Multiple Training Image (MultiTI-MPS) to the Red Dog Deposit Daniel A. Silva and Clayton V. Deutsch A Multiple Point Statistics simulation based on the mixing of two
More informationWaleed Pervaiz CSE 352
Waleed Pervaiz CSE 352 Classification Tool: WEKA Waikato Environment for Knowledge Analysis by The University of Waikato. Available on the internet at: http://www.cs.waikato.ac.nz/~ml/weka/index.html The
More informationA Highly Automatic Petrogeochemistry Diagram Plotting and Analysis System Based on MVVM
2018 International Conference on Computer Science and Software Engineering (CSSE 2018) ISBN: 978-1-60595-555-1 A Highly Automatic Petrogeochemistry Diagram Plotting and Analysis System Based on MVVM Mingguang
More informationA Avenue, Bus: (604) Delta BC V4C 3W2 CANADA Memorandum
11966 95A Avenue, Bus: (604) 582-1100 Delta BC V4C 3W2 CANADA E-mail: trent@sjgeophysics.com www.sjgeophysics.com To: Triple Nine Resources Ltd. Four Corners Mining Corp. Memorandum Attn: Victor French
More informationData Distortion for Privacy Protection in a Terrorist Analysis System
Data Distortion for Privacy Protection in a Terrorist Analysis System Shuting Xu, Jun Zhang, Dianwei Han, and Jie Wang Department of Computer Science, University of Kentucky, Lexington KY 40506-0046, USA
More informationA Geomodeling workflow used to model a complex carbonate reservoir with limited well control : modeling facies zones like fluid zones.
A Geomodeling workflow used to model a complex carbonate reservoir with limited well control : modeling facies zones like fluid zones. Thomas Jerome (RPS), Ke Lovan (WesternZagros) and Suzanne Gentile
More informationMining Engineering Technician: Speciality Mine Exploitation
Mining Engineering Technician: Speciality Mine Exploitation FIRST YEAR PHYSICAL BASES OF ENGINEERING 9220001 Core 1st 1st semester 6 7.2 Mechanics. Electricity. Thermodynamics. Fluid mechanics. Classes
More informationFourier analysis of low-resolution satellite images of cloud
New Zealand Journal of Geology and Geophysics, 1991, Vol. 34: 549-553 0028-8306/91/3404-0549 $2.50/0 Crown copyright 1991 549 Note Fourier analysis of low-resolution satellite images of cloud S. G. BRADLEY
More informationDesign of piezoelectric cantilevers. Tomás Muchenik. MAE 656: Advanced computer aided design Morgantown, WV,
Design of piezoelectric cantilevers Tomás Muchenik MAE 656: Advanced computer aided design Morgantown, WV, 08 10 2012 Presentation Description of the problem solved Description of the numerical model Results
More informationPipeline engineer competency standards list: onshore sector
Pipeline engineer competency standards list: onshore sector ID Competency area/competency Gen Des Cons Ops Level General engineering GE001 Engineering degree in a relevant discipline x Core GE002 Pipeline
More informationValidation and Uncertainty Characterization for Energy Simulation
Validation and Uncertainty Characterization for Energy Simulation Multi-Zone HVAC System using ORNL s Flexible Research Platform (FRP) For: ASHRAE SSPC140 June 26, 2016 PM: Joshua New PIs Piljae Im and
More informationUSE OF DATABASES IN CHARACTERIZATION AT MINE SITES 1
USE OF DATABASES IN CHARACTERIZATION AT MINE SITES 1 Virginia T. McLemore 2, Gretchen K. Hoffman, Maureen Wilks, J. Steven Raugust, and Glen R. Jones Abstract: Mining companies and their consultants generate
More informationSample Introduction Systems SOLID LASER ABLATION -II
Sample Introduction Systems SOLID LASER ABLATION -II Laser ablation systems Variable power output control is an absolute must! This is required in order to achieve a suitable sampling rate, which is dependent
More information3D Equilibrium Reconstruction for Stellarators and Tokamaks
3D Equilibrium Reconstruction for Stellarators and Tokamaks Samuel A. Lazerson 1 D. Gates 1, N. Pablant 1, J. Geiger 2, Y. Suzuki 3, T. Strait 4 [1] Princeton Plasma Physics Laboratory [2] Institute for
More informationAS-i 3.0 Gateways, PROFIsafe via PROFIBUS or PROFINET
safe via or AS-i 3.0 Gateways, safe via or 2 / 1 Master, / Slave AS-i Safety input slaves report via safe AS-i Safety output slaves switch via safe Up to 32 release circuits up to 6 CAT4, SIL 3 safe output
More informationA027 4D Pre-stack Inversion Workflow Integrating Reservoir Model Control and Lithology Supervised Classification
A027 4D Pre-stack Inversion Workflow Integrating Reservoir Model Control and Lithology Supervised Classification S. Toinet* (Total E&P Angola), S. Maultzsch (Total), V. Souvannavong (CGGVeritas) & O. Colnard
More informationIntegration of Geostatistical Modeling with History Matching: Global and Regional Perturbation
Integration of Geostatistical Modeling with History Matching: Global and Regional Perturbation Oliveira, Gonçalo Soares Soares, Amílcar Oliveira (CERENA/IST) Schiozer, Denis José (UNISIM/UNICAMP) Introduction
More informationIntelligent Valve Controller NDX. Safety Manual
Intelligent Valve Controller NDX Safety Manual 10SM NDX en 5/2017 2 Intelligent Valve Controller NDX Safety Manual Table of Contents 1 General information...3 1.1 Purpose of the document... 3 1.2 Description
More informationPROBABILITY OF FAILURE ANALYSIS STANDARDS AND GUIDELINES FOR ELVS
PROBABILITY OF FAILURE ANALYSIS STANDARDS AND GUIDELINES FOR ELVS Federal Aviation Administration 6th IAASS Conference Session 10: Launch Safety Part 1 By:, Elisabeth Morse (Valador Inc.), Paul Rosati
More informationAS-i 3.0 EtherCAT Gateways with integrated Safety Monitor
AS-i 3.0 EtherCAT Gateways with 2 / 1 Master, EtherCat Slave 1 Safety Monitor for 2 s Operation using a single Monitor! Monitor processes safety slaves on two s Coupling between the two networks superfluous
More informationPrograms for MDE Modeling and Conditional Distribution Calculation
Programs for MDE Modeling and Conditional Distribution Calculation Sahyun Hong and Clayton V. Deutsch Improved numerical reservoir models are constructed when all available diverse data sources are accounted
More informationPre-exploitation mesh optimisation in a Nickel deposits (New- Caledonia) Jacques Deraisme (GV), Olivier Bertoli (GV), Jérôme Michaud (SLN)
Pre-exploitation mesh optimisation in a Nickel deposits (New- Caledonia) Jacques Deraisme (GV), Olivier Bertoli (GV), Jérôme Michaud (SLN) 1 Context Optimising drill spacing pattern: a challenging task.
More informationINSTRUCTIONS FOR TYPESETTING MANUSCRIPTS USING TEX OR L A TEX
International Journal of Information Technology & Decision Making c World Scientific Publishing Company INSTRUCTIONS FOR TYPESETTING MANUSCRIPTS USING TEX OR L A TEX FIRST AUTHOR University Department,
More informationA Non-Revenue Water Tale of Five Cities
A Non-Revenue Tale of Five Cities Tory Wagoner, PE/PLS Cavanaugh & Associates, P.A. tory.wagoner@cavanaughsolutions.com 4/25/2017 AWWA M36 Methodology State of the Art Auditing & Loss Control M36 1 st
More informationUsing Blast Data to infer Training Images for MPS Simulation of Continuous Variables
Paper 34, CCG Annual Report 14, 212 ( 212) Using Blast Data to infer Training Images for MPS Simulation of Continuous Variables Hai T. Nguyen and Jeff B. Boisvert Multiple-point simulation (MPS) methods
More informationEffective and Efficient Use of the Fundamentals of Engineering Exam for Outcomes Assessment
Effective and Efficient Use of the Fundamentals of Engineering Exam for Outcomes Assessment Goals/ABET Criteria Addressed The goals of this presentation are to: 1) make participants aware of the changes
More informationA Data estimation Based Approach for Quasi continuous Reservoir Monitoring using Sparse Surface Seismic Data Introduction Figure 1
A Data estimation Based Approach for Quasi continuous Reservoir Monitoring using Sparse Surface Seismic Data Adeyemi Arogunmati* and Jerry M. Harris, Stanford University, California, USA Introduction One
More informationSINUMERIK Safety Integrated. Possible Encoder Connections
SINUMERIK Safety Integrated Possible Encoder Connections siemens.de/safety 1-encoder Safety Servomotor / spindle motor / torque motor SMI DQI 1FW motors 1FW motors 1FW motors Motor with analog interface
More informationA method for inverting ratio-ratio data to estimate end-member. compositions in mixing problems. R. A. Sohn 1
1 2 3 4 A method for inverting ratio-ratio data to estimate end-member compositions in mixing problems R. A. Sohn 1 Woods Hole Oceanographic Institution, Geology & Geophysics Dept., Woods Hole, MA, 02543
More informationRESEARCH ABOUT ROUGHNESS FOR MATING MEMBERS OF A CYLINDRICAL FINE FIT AFTER TURNING WITH SMALL CUTTING FEEDS
International Conference on Economic Engineering and Manufacturing Systems Braşov, 26 27 November 2009 RESEARCH ABOUT ROUGHNESS FOR MATING MEMBERS OF A CYLINDRICAL FINE FIT AFTER TURNING WITH SMALL CUTTING
More informationAnalysis of missing values in simultaneous. functional relationship model for circular variables
Analysis of missing values in simultaneous linear functional relationship model for circular variables S. F. Hassan, Y. Z. Zubairi and A. G. Hussin* Centre for Foundation Studies in Science, University
More informationGravity Methods (VII) wrap up
Environmental and Exploration Geophysics II Gravity Methods (VII) wrap up tom.h.wilson tom.wilson@mail.wvu.edu Department of Geology and Geography West Virginia University Morgantown, WV Items on the list
More informationModeling Uncertainty in the Earth Sciences Jef Caers Stanford University
Modeling spatial continuity Modeling Uncertainty in the Earth Sciences Jef Caers Stanford University Motivation uncertain uncertain certain or uncertain uncertain Spatial Input parameters Spatial Stochastic
More informationA new method for determination of a wave-ray trace based on tsunami isochrones
Bull. Nov. Comp. Center, Math. Model. in Geoph., 13 (2010), 93 101 c 2010 NCC Publisher A new method for determination of a wave-ray trace based on tsunami isochrones An.G. Marchuk Abstract. A new method
More informationSpecial documentation Proline Prowirl 200
SD01204D/06/EN/02.13 71239786 Valid as of version 01.00.zz (Device firmware) Products Solutions Services Special documentation Proline Prowirl 200 Heartbeat Technology Application Package Proline Prowirl
More informationIntroduction to seismic body waves Tomography
Introduction to seismic body waves Tomography Presented by Han Zhang Prepared by group work of Justin Wilgus and Han Zhang Outlines 1. Velocity derived from wave equation 2. Two commonly used reference
More informationInvestigation of mixing chamber for experimental FGD reactor
Investigation of mixing chamber for experimental FGD reactor Jan Novosád 1,a, Petra Danová 1 and Tomáš Vít 1 1 Department of Power Engineering Equipment, Faculty of Mechanical Engineering, Technical University
More informationDeltaV SIS Conditioning Components
DeltaV SIS Process Safety System DeltaV SIS Conditioning Components The DeltaV SIS conditioning components allow you to use the DeltaV SIS system with a variety of different field signal requirements.
More information3D modeling of the Quest Projects Geophysical Datasets. Nigel Phillips
3D modeling of the Quest Projects Geophysical Datasets Nigel Phillips Advanced Geophysical Interpretation Centre Undercover Exploration workshop KEG-25 April 2012 Mineral Physical Properties: density sus.
More informationLoads Recognition Tools Checks Reports
Loads Recognition Tools Checks Reports SDC Verifier is a powerful postprocessor program with an advanced calculation core which works seamlessly with Siemens multi-solver, FEA software suite Femap. SDC
More informationEE360. High-End Moisture in Oil Transmitter. Typical applications. Features EE360 EE360. (+34)
is dedicated for reliable monitoring of lubrication, hydraulic and insulation oils as well as diesel fuel. In addition to highly accurate measurement of water activity (a w ) and temperature (T), calculates
More informationInternational Research Journal of Engineering and Technology (IRJET) e-issn:
SOME NEW OUTCOMES ON PRIME LABELING 1 V. Ganesan & 2 Dr. K. Balamurugan 1 Assistant Professor of Mathematics, T.K. Government Arts College, Vriddhachalam, Tamilnadu 2 Associate Professor of Mathematics,
More informationENDF/B-VII.1 versus ENDFB/-VII.0: What s Different?
LLNL-TR-548633 ENDF/B-VII.1 versus ENDFB/-VII.0: What s Different? by Dermott E. Cullen Lawrence Livermore National Laboratory P.O. Box 808/L-198 Livermore, CA 94550 March 17, 2012 Approved for public
More informationRadio Network Planning with Combinatorial Optimisation Algorithms
Author manuscript, published in "ACTS Mobile Telecommunications Summit 96, Granada : Spain (1996)" Radio Network Planning with Combinatorial Optimisation Algorithms P. Calégari, F. Guidec, P. Kuonen, EPFL,
More informationM. Xie, G. Y. Hong and C. Wohlin, "A Practical Method for the Estimation of Software Reliability Growth in the Early Stage of Testing", Proceedings
M. Xie, G. Y. Hong and C. Wohlin, "A Practical Method for the Estimation of Software Reliability Growth in the Early Stage of Testing", Proceedings IEEE 7th International Symposium on Software Reliability
More informationHardware safety integrity (HSI) in IEC 61508/ IEC 61511
1 Hardware safety integrity (HSI) in IEC 61508/ IEC 61511 ESReDA 2006 June 7-8, 2006 Mary Ann Lundteigen mary.a.lundteigen@ntnu.no mary.a.lundteigen@sintef.no 2 Overview 1. Objective 2. Some concepts &
More informationWelcome to the overview of ACS880 functional safety, FSO-11 Safety functions module.
Welcome to the overview of ACS880 functional safety, FSO-11 Safety functions module. 1 The e-learning sessions about FSO-11 safety functions module contain the following topics. A general overview More
More informationOperating instructions Electronic temperature sensor TN /00 04/2011
Operating instructions Electronic temperature sensor TN7531 UK 704772/00 04/2011 Contents 1 Preliminary note3 1.1 ymbols used 3 2 afety instructions 3 3 Functions and features 4 4 Function 4 4.1 Communication,
More information4D Seismic Inversion on Continuous Land Seismic Reservoir Monitoring of Thermal EOR
4D Seismic Inversion on Continuous Land Seismic Reservoir Monitoring of Thermal EOR Laurene Michou, CGGVeritas, Massy, France, laurene.michou@cggveritas.com Thierry Coleou, CGGVeritas, Massy, France, thierry.coleou@cggveritas.com
More informationAS-i 3.0 Gateways, PROFIsafe via PROFIBUS or PROFINET
via PROFI or PROF AS-i 3.0 Gateways, via PROF or PROFI 22 / 1 Master, PROF / PROFI Slave AS-i Safety input slaves report via AS-i Safety output slaves switch via Up to 32 release circuits up to 6 CAT4,
More informationSeparating the effects of topography and composition. in the Clementine UVVIS data set. Paul Withers - 10 May 1999
Separating the effects of topography and composition in the Clementine UVVIS data set Paul Withers - 10 May 1999 Remote Sensing of Planetary Surfaces Topography and surface composition both affect the
More informationNORAN System 7 Adding value to the Microprobe
NORAN System 7 Adding value to the Microprobe Keith Thompson Introduction The microprobe is a world-class spectroscopic instrument Multiple WDS spectrometers for X-ray detection: Extreme energy resolution
More informationDesign of Surface Seismic Programs for CO2 Storage Monitoring. WesternGeco North America Geophysics Manager Houston
Design of Surface Seismic Programs for CO2 Storage Monitoring Mark S. Egan WesternGeco North America Geophysics Manager Houston Objectives Baseline seismic program Structure & stratigraphy of the storage
More informationRubis (NUM) Tutorial #1
Rubis (NUM) Tutorial #1 1. Introduction This example is an introduction to the basic features of Rubis. The exercise is by no means intended to reproduce a realistic scenario. It is assumed that the user
More informationcv R z design. In this paper, we discuss three of these new methods developed in the last five years.
Nick Moldoveanu, Robin Fletcher, Anthony Lichnewsky, Darrell Coles, WesternGeco Hugues Djikpesse, Schlumberger Doll Research Summary In recent years new methods and tools were developed in seismic survey
More information