The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica

The stratigraphy of the upper part of the Upper Palaeozoic–Lower Mesozoic Victoria Group in the central Transantarctic Mountains is reviewed. Marked lithologic contrasts exist in the Falla Formation between the lower volcanic-poor part and the upper volcaniclastic part. The name Falla Formation is h...

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Published in:Antarctic Science
Main Author: Elliot, D.H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1996
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102096000569
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102096000569
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spelling crcambridgeupr:10.1017/s0954102096000569 2024-09-15T17:48:39+00:00 The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica Elliot, D.H. 1996 http://dx.doi.org/10.1017/s0954102096000569 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102096000569 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 8, issue 4, page 389-394 ISSN 0954-1020 1365-2079 journal-article 1996 crcambridgeupr https://doi.org/10.1017/s0954102096000569 2024-07-31T04:03:51Z The stratigraphy of the upper part of the Upper Palaeozoic–Lower Mesozoic Victoria Group in the central Transantarctic Mountains is reviewed. Marked lithologic contrasts exist in the Falla Formation between the lower volcanic-poor part and the upper volcaniclastic part. The name Falla Formation is here restricted to the lower volcanic-poor part of the sequence making it the youngest formation in the Victoria Group. The upper volcaniclastic part, a tuffaceous sequence, is named the Hanson Formation. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Cambridge University Press Antarctic Science 8 4 389 394
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description The stratigraphy of the upper part of the Upper Palaeozoic–Lower Mesozoic Victoria Group in the central Transantarctic Mountains is reviewed. Marked lithologic contrasts exist in the Falla Formation between the lower volcanic-poor part and the upper volcaniclastic part. The name Falla Formation is here restricted to the lower volcanic-poor part of the sequence making it the youngest formation in the Victoria Group. The upper volcaniclastic part, a tuffaceous sequence, is named the Hanson Formation.
format Article in Journal/Newspaper
author Elliot, D.H.
spellingShingle Elliot, D.H.
The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
author_facet Elliot, D.H.
author_sort Elliot, D.H.
title The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
title_short The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
title_full The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
title_fullStr The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
title_full_unstemmed The Hanson Formation: a new stratigraphical unit in the Transantarctic Mountains, Antarctica
title_sort hanson formation: a new stratigraphical unit in the transantarctic mountains, antarctica
publisher Cambridge University Press (CUP)
publishDate 1996
url http://dx.doi.org/10.1017/s0954102096000569
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102096000569
genre Antarc*
Antarctic Science
Antarctica
genre_facet Antarc*
Antarctic Science
Antarctica
op_source Antarctic Science
volume 8, issue 4, page 389-394
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102096000569
container_title Antarctic Science
container_volume 8
container_issue 4
container_start_page 389
op_container_end_page 394
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