Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica
The Ferrar Large Igneous Province is a widespread magmatic event associated with the break-up of Gondwana during the Jurassic Period. The Ferrar outcrops over a distance of 3000 km throughout the Transantarctic Mountains. It consists of the Ferrar Dolerites, the Dufek intrusion, Kirkpatrick basalts...
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The Ohio State University
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ftohiostateu:oai:kb.osu.edu:1811/59108 2023-05-15T13:43:18+02:00 Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica Harris, Megan C. Elliot, David H. 2014-03 application/pdf http://hdl.handle.net/1811/59108 en_US eng The Ohio State University The Ohio State University. School of Earth Sciences Senior Theses; 2014 http://hdl.handle.net/1811/59108 Antarctica Ferrar Large Igneous Province Geochemistry Thesis 2014 ftohiostateu 2021-01-04T17:57:34Z The Ferrar Large Igneous Province is a widespread magmatic event associated with the break-up of Gondwana during the Jurassic Period. The Ferrar outcrops over a distance of 3000 km throughout the Transantarctic Mountains. It consists of the Ferrar Dolerites, the Dufek intrusion, Kirkpatrick basalts and pyroclastic rocks. Twenty samples collected from Ferrar sills within the Beardmore Glacier region and elsewhere were analyzed to determine the presence of additional olivine-bearing sills and the continuity of the Mount Fazio Chemical Type (MFCT) composition throughout the region. All samples analyzed have been determined to be of the MFCT composition, including a set of samples that are olivine-bearing, and a single sample that belongs to the Dufek intrusion rather than the Ferrar Dolerite. The research expands the geochemical data base and stratigraphic coverage of the Ferrar Large Igneous Province. Arts and Sciences Undergraduate Research Scholarship Shell Exploration and Production Company NSF Grant ANT 0739720 A five-year embargo was granted for this item. Thesis Antarc* Antarctica Beardmore Glacier Ohio State University (OSU): Knowledge Bank Beardmore ENVELOPE(174.900,174.900,-83.350,-83.350) Beardmore Glacier ENVELOPE(170.000,170.000,-84.500,-84.500) Fazio ENVELOPE(162.800,162.800,-73.383,-73.383) Mount Fazio ENVELOPE(162.800,162.800,-73.383,-73.383) Transantarctic Mountains |
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Open Polar |
collection |
Ohio State University (OSU): Knowledge Bank |
op_collection_id |
ftohiostateu |
language |
English |
topic |
Antarctica Ferrar Large Igneous Province Geochemistry |
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Antarctica Ferrar Large Igneous Province Geochemistry Harris, Megan C. Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
topic_facet |
Antarctica Ferrar Large Igneous Province Geochemistry |
description |
The Ferrar Large Igneous Province is a widespread magmatic event associated with the break-up of Gondwana during the Jurassic Period. The Ferrar outcrops over a distance of 3000 km throughout the Transantarctic Mountains. It consists of the Ferrar Dolerites, the Dufek intrusion, Kirkpatrick basalts and pyroclastic rocks. Twenty samples collected from Ferrar sills within the Beardmore Glacier region and elsewhere were analyzed to determine the presence of additional olivine-bearing sills and the continuity of the Mount Fazio Chemical Type (MFCT) composition throughout the region. All samples analyzed have been determined to be of the MFCT composition, including a set of samples that are olivine-bearing, and a single sample that belongs to the Dufek intrusion rather than the Ferrar Dolerite. The research expands the geochemical data base and stratigraphic coverage of the Ferrar Large Igneous Province. Arts and Sciences Undergraduate Research Scholarship Shell Exploration and Production Company NSF Grant ANT 0739720 A five-year embargo was granted for this item. |
author2 |
Elliot, David H. |
format |
Thesis |
author |
Harris, Megan C. |
author_facet |
Harris, Megan C. |
author_sort |
Harris, Megan C. |
title |
Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
title_short |
Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
title_full |
Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
title_fullStr |
Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
title_full_unstemmed |
Geochemistry of some Ferrar Large Igneous Province intrusive rocks in the Transantarctic Mountains, Antarctica |
title_sort |
geochemistry of some ferrar large igneous province intrusive rocks in the transantarctic mountains, antarctica |
publisher |
The Ohio State University |
publishDate |
2014 |
url |
http://hdl.handle.net/1811/59108 |
long_lat |
ENVELOPE(174.900,174.900,-83.350,-83.350) ENVELOPE(170.000,170.000,-84.500,-84.500) ENVELOPE(162.800,162.800,-73.383,-73.383) ENVELOPE(162.800,162.800,-73.383,-73.383) |
geographic |
Beardmore Beardmore Glacier Fazio Mount Fazio Transantarctic Mountains |
geographic_facet |
Beardmore Beardmore Glacier Fazio Mount Fazio Transantarctic Mountains |
genre |
Antarc* Antarctica Beardmore Glacier |
genre_facet |
Antarc* Antarctica Beardmore Glacier |
op_relation |
The Ohio State University. School of Earth Sciences Senior Theses; 2014 http://hdl.handle.net/1811/59108 |
_version_ |
1766187269566234624 |