Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...

The glaucophane schists of Oscar II Land, it has been suggested, originated in a compressive plate boundary subduction zone environment. An alternative hypothesis is presented here linking the metamorphism of these schists with that of the surrounding pre-Carboniferous rocks. It has been estimated f...

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Bibliographic Details
Main Author: Manby, G M
Format: Dataset
Language:English
Published: PANGAEA 1978
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.743267
https://doi.pangaea.de/10.1594/PANGAEA.743267
id ftdatacite:10.1594/pangaea.743267
record_format openpolar
spelling ftdatacite:10.1594/pangaea.743267 2024-09-15T18:29:01+00:00 Tab. 1 Analyses of major phases in Vestgötabreen formation schists ... Manby, G M 1978 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.743267 https://doi.pangaea.de/10.1594/PANGAEA.743267 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Minerals Silicon dioxide Titanium dioxide Aluminium oxide Iron oxide, FeO Manganese oxide Magnesium oxide Calcium oxide Potassium oxide Sodium oxide Elements, total Geological profile sampling Cambridge E.D.S. electron probe microanalyser dataset Supplementary Dataset Dataset 1978 ftdatacite https://doi.org/10.1594/pangaea.743267 2024-08-01T10:57:41Z The glaucophane schists of Oscar II Land, it has been suggested, originated in a compressive plate boundary subduction zone environment. An alternative hypothesis is presented here linking the metamorphism of these schists with that of the surrounding pre-Carboniferous rocks. It has been estimated from mineralogical and textural relationships that at the time of metamorphism these rocks exceeded 30 km in thickness. Similarly, an ambient geothermal gradient of 15° C/km has been calculated for the now exposed succession. Pressures of sufficient magnitude would be realised near the base of this geosynclinal pile to produce eclogite from rocks of basic composition. Subsequent synmetamorphic penetrative deformation would give rise to glaucophane and greenschist facies assemblages. ... : Supplement to: Manby, G M (1978): Aspects of Caledonian metarnorphism in central western Svalbard with particular reference to the Glaucophane schists of Oscar II Land. Polarforschung, 48(1/2), 92-102 ... Dataset Oscar II Land Svalbard DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Minerals
Silicon dioxide
Titanium dioxide
Aluminium oxide
Iron oxide, FeO
Manganese oxide
Magnesium oxide
Calcium oxide
Potassium oxide
Sodium oxide
Elements, total
Geological profile sampling
Cambridge E.D.S. electron probe microanalyser
spellingShingle Minerals
Silicon dioxide
Titanium dioxide
Aluminium oxide
Iron oxide, FeO
Manganese oxide
Magnesium oxide
Calcium oxide
Potassium oxide
Sodium oxide
Elements, total
Geological profile sampling
Cambridge E.D.S. electron probe microanalyser
Manby, G M
Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
topic_facet Minerals
Silicon dioxide
Titanium dioxide
Aluminium oxide
Iron oxide, FeO
Manganese oxide
Magnesium oxide
Calcium oxide
Potassium oxide
Sodium oxide
Elements, total
Geological profile sampling
Cambridge E.D.S. electron probe microanalyser
description The glaucophane schists of Oscar II Land, it has been suggested, originated in a compressive plate boundary subduction zone environment. An alternative hypothesis is presented here linking the metamorphism of these schists with that of the surrounding pre-Carboniferous rocks. It has been estimated from mineralogical and textural relationships that at the time of metamorphism these rocks exceeded 30 km in thickness. Similarly, an ambient geothermal gradient of 15° C/km has been calculated for the now exposed succession. Pressures of sufficient magnitude would be realised near the base of this geosynclinal pile to produce eclogite from rocks of basic composition. Subsequent synmetamorphic penetrative deformation would give rise to glaucophane and greenschist facies assemblages. ... : Supplement to: Manby, G M (1978): Aspects of Caledonian metarnorphism in central western Svalbard with particular reference to the Glaucophane schists of Oscar II Land. Polarforschung, 48(1/2), 92-102 ...
format Dataset
author Manby, G M
author_facet Manby, G M
author_sort Manby, G M
title Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
title_short Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
title_full Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
title_fullStr Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
title_full_unstemmed Tab. 1 Analyses of major phases in Vestgötabreen formation schists ...
title_sort tab. 1 analyses of major phases in vestgötabreen formation schists ...
publisher PANGAEA
publishDate 1978
url https://dx.doi.org/10.1594/pangaea.743267
https://doi.pangaea.de/10.1594/PANGAEA.743267
genre Oscar II Land
Svalbard
genre_facet Oscar II Land
Svalbard
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.743267
_version_ 1810470435004874752