Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains
The sparsity of datable material and key horizons throughout most of the Transantarctic Mountains requires that much of the mapping and correlation of glacial deposits, especially moraines, be based primarily on qualitative techniques. One qualitative method is to characterize the degree of weatheri...
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ftmaineuniv:oai:digitalcommons.library.umaine.edu:ers_facpub-1217 2024-09-15T18:35:47+00:00 Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains Mayewski, Paul Andrew 1976-12-01T08:00:00Z application/pdf https://digitalcommons.library.umaine.edu/ers_facpub/212 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1217/viewcontent/WeatheringStagesofaTholeiiticBasaltDoleriteQueenMaudMountaints.pdf unknown DigitalCommons@UMaine https://digitalcommons.library.umaine.edu/ers_facpub/212 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1217/viewcontent/WeatheringStagesofaTholeiiticBasaltDoleriteQueenMaudMountaints.pdf This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). Earth Science Faculty Scholarship Glaciogeology Geochemistry Glaciology Cryology Climate Change Earth Sciences Hydrology Sedimentology text 1976 ftmaineuniv 2024-07-24T05:38:40Z The sparsity of datable material and key horizons throughout most of the Transantarctic Mountains requires that much of the mapping and correlation of glacial deposits, especially moraines, be based primarily on qualitative techniques. One qualitative method is to characterize the degree of weathering of clasts covering these deposits (Behling, 1971; Calkin, 1971; Nichols, 1971; and Mayewski, 1975). Lacking, however, is a detailed understanding of the role and method of weathering. To help solve this problem, soil studies have been made by Claridge and Campbell (1968) in the Shackleton Glacier region and Everett and Behling (1968), Linkletter (1972), Behling (1971), and Everett (1971) in the dry valleys of southern Victoria Land. Studies on individual lithologies (see,for example, Kelly and Zumberge, 1961) demonstrate the need for more sharply delimited studies,and we are examining a weathering suite of tholeiitic basalts (dolerites) from a site in the Queen Maud Mountains. Text Shackleton Glacier Victoria Land The University of Maine: DigitalCommons@UMaine |
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Open Polar |
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The University of Maine: DigitalCommons@UMaine |
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topic |
Glaciogeology Geochemistry Glaciology Cryology Climate Change Earth Sciences Hydrology Sedimentology |
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Glaciogeology Geochemistry Glaciology Cryology Climate Change Earth Sciences Hydrology Sedimentology Mayewski, Paul Andrew Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
topic_facet |
Glaciogeology Geochemistry Glaciology Cryology Climate Change Earth Sciences Hydrology Sedimentology |
description |
The sparsity of datable material and key horizons throughout most of the Transantarctic Mountains requires that much of the mapping and correlation of glacial deposits, especially moraines, be based primarily on qualitative techniques. One qualitative method is to characterize the degree of weathering of clasts covering these deposits (Behling, 1971; Calkin, 1971; Nichols, 1971; and Mayewski, 1975). Lacking, however, is a detailed understanding of the role and method of weathering. To help solve this problem, soil studies have been made by Claridge and Campbell (1968) in the Shackleton Glacier region and Everett and Behling (1968), Linkletter (1972), Behling (1971), and Everett (1971) in the dry valleys of southern Victoria Land. Studies on individual lithologies (see,for example, Kelly and Zumberge, 1961) demonstrate the need for more sharply delimited studies,and we are examining a weathering suite of tholeiitic basalts (dolerites) from a site in the Queen Maud Mountains. |
format |
Text |
author |
Mayewski, Paul Andrew |
author_facet |
Mayewski, Paul Andrew |
author_sort |
Mayewski, Paul Andrew |
title |
Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
title_short |
Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
title_full |
Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
title_fullStr |
Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
title_full_unstemmed |
Weathering Stages of a Tholeiitic Basalt (Dolerite), Queen Maud Mountains |
title_sort |
weathering stages of a tholeiitic basalt (dolerite), queen maud mountains |
publisher |
DigitalCommons@UMaine |
publishDate |
1976 |
url |
https://digitalcommons.library.umaine.edu/ers_facpub/212 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1217/viewcontent/WeatheringStagesofaTholeiiticBasaltDoleriteQueenMaudMountaints.pdf |
genre |
Shackleton Glacier Victoria Land |
genre_facet |
Shackleton Glacier Victoria Land |
op_source |
Earth Science Faculty Scholarship |
op_relation |
https://digitalcommons.library.umaine.edu/ers_facpub/212 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1217/viewcontent/WeatheringStagesofaTholeiiticBasaltDoleriteQueenMaudMountaints.pdf |
op_rights |
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). |
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