Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway
Carbonate-orthopyroxenites from Troms consist of enstatite and magnesite with variable amounts of olivine, talc, serpentine, chlorite, and phlogopite and include the ore minerals chromite, magnetite, pentlandite, pyrite, and in some cases pyrrhotite, heazlewoodite, millerite, and maucherite. Related...
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fthighwire:oai:open-archive.highwire.org:petrology:15/2/303 2023-05-15T17:43:29+02:00 Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway OHNMACHT, W. 1974-01-01 00:00:00.0 text/html http://petrology.oxfordjournals.org/cgi/content/short/15/2/303 https://doi.org/10.1093/petrology/15.2.303 en eng Oxford University Press http://petrology.oxfordjournals.org/cgi/content/short/15/2/303 http://dx.doi.org/10.1093/petrology/15.2.303 Copyright (C) 1974, Oxford University Press Articles TEXT 1974 fthighwire https://doi.org/10.1093/petrology/15.2.303 2015-03-01T00:44:48Z Carbonate-orthopyroxenites from Troms consist of enstatite and magnesite with variable amounts of olivine, talc, serpentine, chlorite, and phlogopite and include the ore minerals chromite, magnetite, pentlandite, pyrite, and in some cases pyrrhotite, heazlewoodite, millerite, and maucherite. Related rocks comprise olivine-magnesite-, talc-magnesite and olivine-orthopyroxene (saxonite)-assemblages. Allochemical replacement reactions, involving mobile CO 2 , H 2 O, and SiO 2 , are shown to comprise the main petrogenetic mechanism. Saxonite, however, may represent a possible source material. Discussion of the model system MgO-SiO 2 -CO 2 -H 2 O for P flukl = 2 and 7 kb, respectively, indicates that best agreement with petrographic evidence is reached assuming elevated pressures and both gas-excess and gas-deficiency conditions by means of local equilibria. The gas-deficient assemblage enstatite+talc+forsterite+magnesite is presumed to be stable at pressures above 5 kb. Recalculation of whole-rock analyses to a CO 2 -free basis by several alternative methods suggests that rock evolution could have followed the trend dunite↑ saxonite↑ orthopyroxenite↑ sagvandite+related rocks. A simple geometric method is used to outline possible schemes of rock evolution, involving gas-deficient phase assemblages. Text Northern Norway Troms HighWire Press (Stanford University) Norway Journal of Petrology 15 2 303 324 |
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Articles OHNMACHT, W. Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
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description |
Carbonate-orthopyroxenites from Troms consist of enstatite and magnesite with variable amounts of olivine, talc, serpentine, chlorite, and phlogopite and include the ore minerals chromite, magnetite, pentlandite, pyrite, and in some cases pyrrhotite, heazlewoodite, millerite, and maucherite. Related rocks comprise olivine-magnesite-, talc-magnesite and olivine-orthopyroxene (saxonite)-assemblages. Allochemical replacement reactions, involving mobile CO 2 , H 2 O, and SiO 2 , are shown to comprise the main petrogenetic mechanism. Saxonite, however, may represent a possible source material. Discussion of the model system MgO-SiO 2 -CO 2 -H 2 O for P flukl = 2 and 7 kb, respectively, indicates that best agreement with petrographic evidence is reached assuming elevated pressures and both gas-excess and gas-deficiency conditions by means of local equilibria. The gas-deficient assemblage enstatite+talc+forsterite+magnesite is presumed to be stable at pressures above 5 kb. Recalculation of whole-rock analyses to a CO 2 -free basis by several alternative methods suggests that rock evolution could have followed the trend dunite↑ saxonite↑ orthopyroxenite↑ sagvandite+related rocks. A simple geometric method is used to outline possible schemes of rock evolution, involving gas-deficient phase assemblages. |
format |
Text |
author |
OHNMACHT, W. |
author_facet |
OHNMACHT, W. |
author_sort |
OHNMACHT, W. |
title |
Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
title_short |
Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
title_full |
Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
title_fullStr |
Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
title_full_unstemmed |
Petrogenesis of Carbonate-orthopyroxenites (Sagvandites) and related rocks from Troms, Northern Norway |
title_sort |
petrogenesis of carbonate-orthopyroxenites (sagvandites) and related rocks from troms, northern norway |
publisher |
Oxford University Press |
publishDate |
1974 |
url |
http://petrology.oxfordjournals.org/cgi/content/short/15/2/303 https://doi.org/10.1093/petrology/15.2.303 |
geographic |
Norway |
geographic_facet |
Norway |
genre |
Northern Norway Troms |
genre_facet |
Northern Norway Troms |
op_relation |
http://petrology.oxfordjournals.org/cgi/content/short/15/2/303 http://dx.doi.org/10.1093/petrology/15.2.303 |
op_rights |
Copyright (C) 1974, Oxford University Press |
op_doi |
https://doi.org/10.1093/petrology/15.2.303 |
container_title |
Journal of Petrology |
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15 |
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2 |
container_start_page |
303 |
op_container_end_page |
324 |
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1766145571634020352 |