Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica

The Fremouw and Falla Formations are part of a thick sequence of alluvial sediments that accumulated in a foreland basin (foredeep) between the Antarctic craton and the Gondwanian orogen, an Andean-type mountain belt along the Pacific margin of Gondwana. This study examines the petrology of Fremouw...

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Bibliographic Details
Main Author: Vavra, Charles L.
Format: Report
Language:English
Published: Institute of Polar Studies, The Ohio State University. 1984
Subjects:
Beacon Supergroup
Transantarctic Mountains
Antarctica
Falla Formation
Fremouw Formation
Antarctic
Cumulus Hills
Falla
Pacific
The Antarctic
Antarc*
Online Access:http://hdl.handle.net/1811/48692
id ftohiostateu:oai:kb.osu.edu:1811/48692
record_format openpolar
spelling ftohiostateu:oai:kb.osu.edu:1811/48692 2023-05-15T13:40:53+02:00 Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica Vavra, Charles L. 1984 application/pdf http://hdl.handle.net/1811/48692 en_US eng Institute of Polar Studies, The Ohio State University. Institute of Polar Studies Report 87 Vavra, Charles L. 1984. Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica. Institute of Polar Studies Report 87, Institute of Polar Studies, The Ohio State University, Columbus, 98 pages. 0078-415X http://hdl.handle.net/1811/48692 Beacon Supergroup Transantarctic Mountains Antarctica Falla Formation Fremouw Formation Technical Report 1984 ftohiostateu 2020-08-22T19:06:41Z The Fremouw and Falla Formations are part of a thick sequence of alluvial sediments that accumulated in a foreland basin (foredeep) between the Antarctic craton and the Gondwanian orogen, an Andean-type mountain belt along the Pacific margin of Gondwana. This study examines the petrology of Fremouw and Falla sandstone in the central Transantarctic Mountains from the Cumulus Hills to the Queen Alexandra Range in order to determine provenance and post-depositional history. Digenetic Modeling Group, Geological Research, Arco Oil and Gas Company, Dallas, TX Report Antarc* Antarctic Antarctica Ohio State University (OSU): Knowledge Bank Antarctic Cumulus Hills ENVELOPE(-175.000,-175.000,-85.333,-85.333) Falla ENVELOPE(164.917,164.917,-84.367,-84.367) Pacific The Antarctic Transantarctic Mountains
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
topic Beacon Supergroup
Transantarctic Mountains
Antarctica
Falla Formation
Fremouw Formation
spellingShingle Beacon Supergroup
Transantarctic Mountains
Antarctica
Falla Formation
Fremouw Formation
Vavra, Charles L.
Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
topic_facet Beacon Supergroup
Transantarctic Mountains
Antarctica
Falla Formation
Fremouw Formation
description The Fremouw and Falla Formations are part of a thick sequence of alluvial sediments that accumulated in a foreland basin (foredeep) between the Antarctic craton and the Gondwanian orogen, an Andean-type mountain belt along the Pacific margin of Gondwana. This study examines the petrology of Fremouw and Falla sandstone in the central Transantarctic Mountains from the Cumulus Hills to the Queen Alexandra Range in order to determine provenance and post-depositional history. Digenetic Modeling Group, Geological Research, Arco Oil and Gas Company, Dallas, TX
format Report
author Vavra, Charles L.
author_facet Vavra, Charles L.
author_sort Vavra, Charles L.
title Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
title_short Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
title_full Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
title_fullStr Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
title_full_unstemmed Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica
title_sort provenance and alteration of the triassic fremouw and falla formations, central transantarctic mountains, antarctica
publisher Institute of Polar Studies, The Ohio State University.
publishDate 1984
url http://hdl.handle.net/1811/48692
long_lat ENVELOPE(-175.000,-175.000,-85.333,-85.333)
ENVELOPE(164.917,164.917,-84.367,-84.367)
geographic Antarctic
Cumulus Hills
Falla
Pacific
The Antarctic
Transantarctic Mountains
geographic_facet Antarctic
Cumulus Hills
Falla
Pacific
The Antarctic
Transantarctic Mountains
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation Institute of Polar Studies Report 87
Vavra, Charles L. 1984. Provenance and Alteration of the Triassic Fremouw and Falla Formations, Central Transantarctic Mountains, Antarctica. Institute of Polar Studies Report 87, Institute of Polar Studies, The Ohio State University, Columbus, 98 pages.
0078-415X
http://hdl.handle.net/1811/48692
_version_ 1766142403232661504

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