Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2)
One of the objectives of the Cape Roberts Project is to study the tectonic history of the western Ross Sea region. Timing of the uplift of the Transantarctic Mountains, which are adjacent to the drillsite, will be a component of the tectonic studies (International Steering Committee, 1994; Cale Robe...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.54734 2023-05-15T14:04:42+02:00 Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) Kyle, Philip R LATITUDE: -77.007580 * LONGITUDE: 163.755080 * DATE/TIME START: 1997-10-17T01:30:00 * DATE/TIME END: 1997-10-24T02:00:00 * MINIMUM DEPTH, sediment/rock: 21.84 m * MAXIMUM DEPTH, sediment/rock: 137.16 m 1998-01-15 text/tab-separated-values, 276 data points https://doi.pangaea.de/10.1594/PANGAEA.54734 https://doi.org/10.1594/PANGAEA.54734 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.54734 https://doi.org/10.1594/PANGAEA.54734 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Kyle, Philip R (1998): Ferrar dolerite clasts from CRP-1 drillcore. Terra Antartica, 5(3), 611-612, hdl:10013/epic.28324.d001 16 km ENE Cape Roberts Aluminium oxide Barium Calcium oxide Cape Roberts Project Chromium Comment Copper Core wireline system CRP CRP-1 CWS DEPTH sediment/rock Gallium Iron oxide Fe2O3 Lead Loss on ignition Magnesium oxide Manganese oxide Nickel Niobium off Cape Roberts Ross Sea Antarctica Phosphorus oxide Potassium oxide Rubidium Sample volume Sampling/drilling ice Silicon dioxide Sodium oxide Strontium Sum Thorium Titanium dioxide Uranium Vanadium X-ray fluorescence (XRF) Yttrium Zinc Zirconium Dataset 1998 ftpangaea https://doi.org/10.1594/PANGAEA.54734 2023-01-20T07:35:43Z One of the objectives of the Cape Roberts Project is to study the tectonic history of the western Ross Sea region. Timing of the uplift of the Transantarctic Mountains, which are adjacent to the drillsite, will be a component of the tectonic studies (International Steering Committee, 1994; Cale Roberts Science Team, 1998a). The study of the clast samples from the core will be an important means of providing insight into the timing of uplift of the Transantarctic Mountains. Tholeiitic igneous rocks of the Jurassic (180 Ma) Ferrar large igneous province (FLIP) are widespreaded along the Transantarctic Mountains and have the potential to provide distinct indicators of erosion during uplift of the mountains. In the Transantarctic Mountains adjacent to the Cape Roberts drill site the FLIP is represented by lavas and pyroclastic of the Kirkpatrick basalts and by thick Ferrar dolerite sills which intrude the Beacon Supergroup sediments and, occasionally, the granitic basement rocks. In the Prince Albert Mountains, the youngest Kirkpatrick basalt lava is over 150 m thick, and has a very distinct high TiO2 chemical composition which is unique in the FLIP. If such rocks can be identified in the core they may provide precise timing of the initiation of uplift and denudation of the Transantarctic Mountains. Here we report on an examination of 20 Ferrar dolerite clasts. This brief report is intended as a pilot study to the examination of FLIP clasts from older drillcore. Dataset Antarc* Antarctica Ross Sea PANGAEA - Data Publisher for Earth & Environmental Science Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) Prince Albert Mountains ENVELOPE(161.500,161.500,-76.000,-76.000) Ross Sea Transantarctic Mountains ENVELOPE(163.755080,163.755080,-77.007580,-77.007580) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
16 km ENE Cape Roberts Aluminium oxide Barium Calcium oxide Cape Roberts Project Chromium Comment Copper Core wireline system CRP CRP-1 CWS DEPTH sediment/rock Gallium Iron oxide Fe2O3 Lead Loss on ignition Magnesium oxide Manganese oxide Nickel Niobium off Cape Roberts Ross Sea Antarctica Phosphorus oxide Potassium oxide Rubidium Sample volume Sampling/drilling ice Silicon dioxide Sodium oxide Strontium Sum Thorium Titanium dioxide Uranium Vanadium X-ray fluorescence (XRF) Yttrium Zinc Zirconium |
spellingShingle |
16 km ENE Cape Roberts Aluminium oxide Barium Calcium oxide Cape Roberts Project Chromium Comment Copper Core wireline system CRP CRP-1 CWS DEPTH sediment/rock Gallium Iron oxide Fe2O3 Lead Loss on ignition Magnesium oxide Manganese oxide Nickel Niobium off Cape Roberts Ross Sea Antarctica Phosphorus oxide Potassium oxide Rubidium Sample volume Sampling/drilling ice Silicon dioxide Sodium oxide Strontium Sum Thorium Titanium dioxide Uranium Vanadium X-ray fluorescence (XRF) Yttrium Zinc Zirconium Kyle, Philip R Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
topic_facet |
16 km ENE Cape Roberts Aluminium oxide Barium Calcium oxide Cape Roberts Project Chromium Comment Copper Core wireline system CRP CRP-1 CWS DEPTH sediment/rock Gallium Iron oxide Fe2O3 Lead Loss on ignition Magnesium oxide Manganese oxide Nickel Niobium off Cape Roberts Ross Sea Antarctica Phosphorus oxide Potassium oxide Rubidium Sample volume Sampling/drilling ice Silicon dioxide Sodium oxide Strontium Sum Thorium Titanium dioxide Uranium Vanadium X-ray fluorescence (XRF) Yttrium Zinc Zirconium |
description |
One of the objectives of the Cape Roberts Project is to study the tectonic history of the western Ross Sea region. Timing of the uplift of the Transantarctic Mountains, which are adjacent to the drillsite, will be a component of the tectonic studies (International Steering Committee, 1994; Cale Roberts Science Team, 1998a). The study of the clast samples from the core will be an important means of providing insight into the timing of uplift of the Transantarctic Mountains. Tholeiitic igneous rocks of the Jurassic (180 Ma) Ferrar large igneous province (FLIP) are widespreaded along the Transantarctic Mountains and have the potential to provide distinct indicators of erosion during uplift of the mountains. In the Transantarctic Mountains adjacent to the Cape Roberts drill site the FLIP is represented by lavas and pyroclastic of the Kirkpatrick basalts and by thick Ferrar dolerite sills which intrude the Beacon Supergroup sediments and, occasionally, the granitic basement rocks. In the Prince Albert Mountains, the youngest Kirkpatrick basalt lava is over 150 m thick, and has a very distinct high TiO2 chemical composition which is unique in the FLIP. If such rocks can be identified in the core they may provide precise timing of the initiation of uplift and denudation of the Transantarctic Mountains. Here we report on an examination of 20 Ferrar dolerite clasts. This brief report is intended as a pilot study to the examination of FLIP clasts from older drillcore. |
format |
Dataset |
author |
Kyle, Philip R |
author_facet |
Kyle, Philip R |
author_sort |
Kyle, Philip R |
title |
Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
title_short |
Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
title_full |
Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
title_fullStr |
Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
title_full_unstemmed |
Selected major elements and trace elements of ferrar dolerite clasts from sediment core CRP-1 (Table 1,2) |
title_sort |
selected major elements and trace elements of ferrar dolerite clasts from sediment core crp-1 (table 1,2) |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.54734 https://doi.org/10.1594/PANGAEA.54734 |
op_coverage |
LATITUDE: -77.007580 * LONGITUDE: 163.755080 * DATE/TIME START: 1997-10-17T01:30:00 * DATE/TIME END: 1997-10-24T02:00:00 * MINIMUM DEPTH, sediment/rock: 21.84 m * MAXIMUM DEPTH, sediment/rock: 137.16 m |
long_lat |
ENVELOPE(-70.467,-70.467,-68.950,-68.950) ENVELOPE(161.500,161.500,-76.000,-76.000) ENVELOPE(163.755080,163.755080,-77.007580,-77.007580) |
geographic |
Cape Roberts Prince Albert Mountains Ross Sea Transantarctic Mountains |
geographic_facet |
Cape Roberts Prince Albert Mountains Ross Sea Transantarctic Mountains |
genre |
Antarc* Antarctica Ross Sea |
genre_facet |
Antarc* Antarctica Ross Sea |
op_source |
Supplement to: Kyle, Philip R (1998): Ferrar dolerite clasts from CRP-1 drillcore. Terra Antartica, 5(3), 611-612, hdl:10013/epic.28324.d001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.54734 https://doi.org/10.1594/PANGAEA.54734 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.54734 |
_version_ |
1766275939924180992 |