Geochemistry on rocks from the eastern Weddell Sea ...

Petrographie and geochemical investigations on ice-rafted debris along the continental margin of the eastern and southern Weddell Sea give additional information for modelling subglacial geology at the continental border region. From northeast to southwest five provinces with different petrographic...

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Main Author: Oskierski, Wolfgang
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1988
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.884518
https://doi.pangaea.de/10.1594/PANGAEA.884518
id ftdatacite:10.1594/pangaea.884518
record_format openpolar
spelling ftdatacite:10.1594/pangaea.884518 2024-09-09T19:11:19+00:00 Geochemistry on rocks from the eastern Weddell Sea ... Oskierski, Wolfgang 1988 application/zip https://dx.doi.org/10.1594/pangaea.884518 https://doi.pangaea.de/10.1594/PANGAEA.884518 en eng PANGAEA https://dx.doi.org/10.2312/bzp_0047_1988 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 1988 ftdatacite https://doi.org/10.1594/pangaea.88451810.2312/bzp_0047_1988 2024-08-01T10:53:02Z Petrographie and geochemical investigations on ice-rafted debris along the continental margin of the eastern and southern Weddell Sea give additional information for modelling subglacial geology at the continental border region. From northeast to southwest five provinces with different petrographic and geochemical properties could be distinguished:The northeastern Province I is characterized by volcanic rocks, mainly basalts (>90 %). 0nly a small portion of clastic sedimentary rocks was recognized while metamorphic and plutonic rocks are almost lacking.Province II is still dominated by basaltic rocks (60 %), but there is a considerable increase in metamorphic (15 %) and clastic seedimentary rocks (25 %).Province III is typified by a variation in the occurrence of medium to high grade metamorphics (36 %) and a variety of different plutonic rocks (30 %). The portion of volcanic rocks decrease to 20 % whereas sedimentary rocks form a portion of 13 %.Almost equal portions of intermediate to acidic plutonic ... : Supplement to: Oskierski, Wolfgang (1988): Verteilung und Herkunft glazial-mariner Gerölle am Antarktischen Kontinentalrand des östlichen Weddellmeeres = Distribution and orgin of glaciomarine pebbles on the Antarctic continental margin of the Eastern Weddell Sea. Berichte zur Polarforschung = Reports on Polar Research, 47, 167 pp ... Article in Journal/Newspaper Antarc* Antarctic Antarktis* Weddell Sea DataCite Antarctic The Antarctic Weddell Sea Weddell
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Oskierski, Wolfgang
Geochemistry on rocks from the eastern Weddell Sea ...
topic_facet Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Petrographie and geochemical investigations on ice-rafted debris along the continental margin of the eastern and southern Weddell Sea give additional information for modelling subglacial geology at the continental border region. From northeast to southwest five provinces with different petrographic and geochemical properties could be distinguished:The northeastern Province I is characterized by volcanic rocks, mainly basalts (>90 %). 0nly a small portion of clastic sedimentary rocks was recognized while metamorphic and plutonic rocks are almost lacking.Province II is still dominated by basaltic rocks (60 %), but there is a considerable increase in metamorphic (15 %) and clastic seedimentary rocks (25 %).Province III is typified by a variation in the occurrence of medium to high grade metamorphics (36 %) and a variety of different plutonic rocks (30 %). The portion of volcanic rocks decrease to 20 % whereas sedimentary rocks form a portion of 13 %.Almost equal portions of intermediate to acidic plutonic ... : Supplement to: Oskierski, Wolfgang (1988): Verteilung und Herkunft glazial-mariner Gerölle am Antarktischen Kontinentalrand des östlichen Weddellmeeres = Distribution and orgin of glaciomarine pebbles on the Antarctic continental margin of the Eastern Weddell Sea. Berichte zur Polarforschung = Reports on Polar Research, 47, 167 pp ...
format Article in Journal/Newspaper
author Oskierski, Wolfgang
author_facet Oskierski, Wolfgang
author_sort Oskierski, Wolfgang
title Geochemistry on rocks from the eastern Weddell Sea ...
title_short Geochemistry on rocks from the eastern Weddell Sea ...
title_full Geochemistry on rocks from the eastern Weddell Sea ...
title_fullStr Geochemistry on rocks from the eastern Weddell Sea ...
title_full_unstemmed Geochemistry on rocks from the eastern Weddell Sea ...
title_sort geochemistry on rocks from the eastern weddell sea ...
publisher PANGAEA
publishDate 1988
url https://dx.doi.org/10.1594/pangaea.884518
https://doi.pangaea.de/10.1594/PANGAEA.884518
geographic Antarctic
The Antarctic
Weddell Sea
Weddell
geographic_facet Antarctic
The Antarctic
Weddell Sea
Weddell
genre Antarc*
Antarctic
Antarktis*
Weddell Sea
genre_facet Antarc*
Antarctic
Antarktis*
Weddell Sea
op_relation https://dx.doi.org/10.2312/bzp_0047_1988
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.88451810.2312/bzp_0047_1988
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