Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India
Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mishra, B. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1988 |
|---|
| Schlagwörter: |
|---|
| Systematik: |
|
|---|
| Anmerkung: |
© Springer-Verlag 1988 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Mineralium deposita - Springer-Verlag, 1966, 23(1988), 3 vom: Juli, Seite 179-185 |
|---|---|
| Übergeordnetes Werk: |
volume:23 ; year:1988 ; number:3 ; month:07 ; pages:179-185 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00204298 |
|---|
| Katalog-ID: |
OLC205824284X |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC205824284X | ||
| 003 | DE-627 | ||
| 005 | 20230401050123.0 | ||
| 007 | tu | ||
| 008 | 200820s1988 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/BF00204298 |2 doi | |
| 035 | |a (DE-627)OLC205824284X | ||
| 035 | |a (DE-He213)BF00204298-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 13 |2 ssgn | ||
| 084 | |a TE 1000 |q VZ |2 rvk | ||
| 100 | 1 | |a Mishra, B. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| 264 | 1 | |c 1988 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Springer-Verlag 1988 | ||
| 520 | |a Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. | ||
| 650 | 4 | |a Sulfide | |
| 650 | 4 | |a Fractionation | |
| 650 | 4 | |a Fluid Inclusion | |
| 650 | 4 | |a Distribution Coefficient | |
| 650 | 4 | |a Subtle Change | |
| 700 | 1 | |a Mookherjee, A. |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Mineralium deposita |d Springer-Verlag, 1966 |g 23(1988), 3 vom: Juli, Seite 179-185 |w (DE-627)12906906X |w (DE-600)1679-2 |w (DE-576)01440074X |x 0026-4598 |7 nnns |
| 773 | 1 | 8 | |g volume:23 |g year:1988 |g number:3 |g month:07 |g pages:179-185 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/BF00204298 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_11 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_30 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_65 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_2004 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2015 | ||
| 912 | |a GBV_ILN_2018 | ||
| 912 | |a GBV_ILN_2027 | ||
| 912 | |a GBV_ILN_4036 | ||
| 912 | |a GBV_ILN_4037 | ||
| 912 | |a GBV_ILN_4046 | ||
| 912 | |a GBV_ILN_4082 | ||
| 912 | |a GBV_ILN_4103 | ||
| 912 | |a GBV_ILN_4112 | ||
| 912 | |a GBV_ILN_4125 | ||
| 912 | |a GBV_ILN_4305 | ||
| 912 | |a GBV_ILN_4306 | ||
| 912 | |a GBV_ILN_4307 | ||
| 912 | |a GBV_ILN_4319 | ||
| 912 | |a GBV_ILN_4323 | ||
| 936 | r | v | |a TE 1000 |
| 951 | |a AR | ||
| 952 | |d 23 |j 1988 |e 3 |c 07 |h 179-185 | ||
| author_variant |
b m bm a m am |
|---|---|
| matchkey_str |
article:00264598:1988----::etemmtyaeofatoainfnncbtenoxsigpaeienglnfosmcro |
| hierarchy_sort_str |
1988 |
| publishDate |
1988 |
| allfields |
10.1007/BF00204298 doi (DE-627)OLC205824284X (DE-He213)BF00204298-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Mishra, B. verfasserin aut Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1988 Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change Mookherjee, A. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 23(1988), 3 vom: Juli, Seite 179-185 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:23 year:1988 number:3 month:07 pages:179-185 https://doi.org/10.1007/BF00204298 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 23 1988 3 07 179-185 |
| spelling |
10.1007/BF00204298 doi (DE-627)OLC205824284X (DE-He213)BF00204298-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Mishra, B. verfasserin aut Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1988 Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change Mookherjee, A. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 23(1988), 3 vom: Juli, Seite 179-185 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:23 year:1988 number:3 month:07 pages:179-185 https://doi.org/10.1007/BF00204298 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 23 1988 3 07 179-185 |
| allfields_unstemmed |
10.1007/BF00204298 doi (DE-627)OLC205824284X (DE-He213)BF00204298-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Mishra, B. verfasserin aut Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1988 Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change Mookherjee, A. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 23(1988), 3 vom: Juli, Seite 179-185 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:23 year:1988 number:3 month:07 pages:179-185 https://doi.org/10.1007/BF00204298 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 23 1988 3 07 179-185 |
| allfieldsGer |
10.1007/BF00204298 doi (DE-627)OLC205824284X (DE-He213)BF00204298-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Mishra, B. verfasserin aut Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1988 Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change Mookherjee, A. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 23(1988), 3 vom: Juli, Seite 179-185 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:23 year:1988 number:3 month:07 pages:179-185 https://doi.org/10.1007/BF00204298 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 23 1988 3 07 179-185 |
| allfieldsSound |
10.1007/BF00204298 doi (DE-627)OLC205824284X (DE-He213)BF00204298-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Mishra, B. verfasserin aut Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1988 Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change Mookherjee, A. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 23(1988), 3 vom: Juli, Seite 179-185 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:23 year:1988 number:3 month:07 pages:179-185 https://doi.org/10.1007/BF00204298 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 23 1988 3 07 179-185 |
| language |
English |
| source |
Enthalten in Mineralium deposita 23(1988), 3 vom: Juli, Seite 179-185 volume:23 year:1988 number:3 month:07 pages:179-185 |
| sourceStr |
Enthalten in Mineralium deposita 23(1988), 3 vom: Juli, Seite 179-185 volume:23 year:1988 number:3 month:07 pages:179-185 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Mineralium deposita |
| authorswithroles_txt_mv |
Mishra, B. @@aut@@ Mookherjee, A. @@aut@@ |
| publishDateDaySort_date |
1988-07-01T00:00:00Z |
| hierarchy_top_id |
12906906X |
| dewey-sort |
3550 |
| id |
OLC205824284X |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC205824284X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401050123.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s1988 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00204298</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC205824284X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00204298-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TE 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mishra, B.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1988</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 1988</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sulfide</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fractionation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fluid Inclusion</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Distribution Coefficient</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subtle Change</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mookherjee, A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Mineralium deposita</subfield><subfield code="d">Springer-Verlag, 1966</subfield><subfield code="g">23(1988), 3 vom: Juli, Seite 179-185</subfield><subfield code="w">(DE-627)12906906X</subfield><subfield code="w">(DE-600)1679-2</subfield><subfield code="w">(DE-576)01440074X</subfield><subfield code="x">0026-4598</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:23</subfield><subfield code="g">year:1988</subfield><subfield code="g">number:3</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:179-185</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00204298</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4036</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4082</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4103</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4319</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">TE 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">23</subfield><subfield code="j">1988</subfield><subfield code="e">3</subfield><subfield code="c">07</subfield><subfield code="h">179-185</subfield></datafield></record></collection>
|
| author |
Mishra, B. |
| spellingShingle |
Mishra, B. ddc 550 ssgn 13 rvk TE 1000 misc Sulfide misc Fractionation misc Fluid Inclusion misc Distribution Coefficient misc Subtle Change Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| authorStr |
Mishra, B. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)12906906X |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0026-4598 |
| topic_title |
550 VZ 13 ssgn TE 1000 VZ rvk Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India Sulfide Fractionation Fluid Inclusion Distribution Coefficient Subtle Change |
| topic |
ddc 550 ssgn 13 rvk TE 1000 misc Sulfide misc Fractionation misc Fluid Inclusion misc Distribution Coefficient misc Subtle Change |
| topic_unstemmed |
ddc 550 ssgn 13 rvk TE 1000 misc Sulfide misc Fractionation misc Fluid Inclusion misc Distribution Coefficient misc Subtle Change |
| topic_browse |
ddc 550 ssgn 13 rvk TE 1000 misc Sulfide misc Fractionation misc Fluid Inclusion misc Distribution Coefficient misc Subtle Change |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Mineralium deposita |
| hierarchy_parent_id |
12906906X |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Mineralium deposita |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X |
| title |
Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| ctrlnum |
(DE-627)OLC205824284X (DE-He213)BF00204298-p |
| title_full |
Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| author_sort |
Mishra, B. |
| journal |
Mineralium deposita |
| journalStr |
Mineralium deposita |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
1988 |
| contenttype_str_mv |
txt |
| container_start_page |
179 |
| author_browse |
Mishra, B. Mookherjee, A. |
| container_volume |
23 |
| class |
550 VZ 13 ssgn TE 1000 VZ rvk |
| format_se |
Aufsätze |
| author-letter |
Mishra, B. |
| doi_str_mv |
10.1007/BF00204298 |
| dewey-full |
550 |
| title_sort |
geothermometry based on fractionation of mn and cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in india |
| title_auth |
Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| abstract |
Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. © Springer-Verlag 1988 |
| abstractGer |
Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. © Springer-Verlag 1988 |
| abstract_unstemmed |
Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism. © Springer-Verlag 1988 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 |
| container_issue |
3 |
| title_short |
Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India |
| url |
https://doi.org/10.1007/BF00204298 |
| remote_bool |
false |
| author2 |
Mookherjee, A. |
| author2Str |
Mookherjee, A. |
| ppnlink |
12906906X |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/BF00204298 |
| up_date |
2024-07-03T18:13:18.356Z |
| _version_ |
1803582594989686784 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC205824284X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401050123.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s1988 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00204298</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC205824284X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00204298-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TE 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mishra, B.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Geothermometry based on fractionation of Mn and Cd between coexisting sphalerite and galena from some carbonate-hosted sulfide deposits in India</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1988</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 1988</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Geothermometry based on the fractionation of Mn and Cd between coexisting sphalerite and galena from concordantly banded, strata-bound ores and younger vein ores of Rajpura-Dariba, Zawar, and Bandalamottu has been attempted. Different fractionation trends for the banded and vein ores in the same deposit at Rajpura-Dariba indicate different thermal regimes of final equilibration for the two varieties of ores. In contrast, a single trend incorporating both types of ores is suggestive of isothermal conditions of final equilibration for the banded and vein ores at Zawar. Unrealistically high temperatures obtained for the vein ores of Bandalamottu suggest equilibrium in the sphalerite-galena aggregates of this deposit was not attained. Thermometric data from Mn and Cd fractionation are compared with other independent geothermometric determinations obtained from fluid inclusion homogenization studies and based on phase equilibria. It has been found that, in general, the Cd-fractionation temperature ($ T_{Cd} $) is a more reliable geothermometer than the Mn-fractionation temperature ($ T_{Mn} $). This presumably may be due to the susceptibility of aqueous Mn species to subtle changes in $$f_{O_2 } $$ in the ore fluid and consequent heterogeneity in Mn concentration in sphalerite, thus affecting the distribution coefficient. The investigation also suggests that $ T_{Cd} $ becomes increasingly more dependable when the ores are metamorphosed and reequilibrated at higher grades of metamorphism.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sulfide</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fractionation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fluid Inclusion</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Distribution Coefficient</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subtle Change</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mookherjee, A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Mineralium deposita</subfield><subfield code="d">Springer-Verlag, 1966</subfield><subfield code="g">23(1988), 3 vom: Juli, Seite 179-185</subfield><subfield code="w">(DE-627)12906906X</subfield><subfield code="w">(DE-600)1679-2</subfield><subfield code="w">(DE-576)01440074X</subfield><subfield code="x">0026-4598</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:23</subfield><subfield code="g">year:1988</subfield><subfield code="g">number:3</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:179-185</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00204298</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4036</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4082</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4103</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4319</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">TE 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">23</subfield><subfield code="j">1988</subfield><subfield code="e">3</subfield><subfield code="c">07</subfield><subfield code="h">179-185</subfield></datafield></record></collection>
|
| score |
7.4011087 |