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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Bibliographic Details
Main Author: Kyle, Philip R
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
Sum
Online Access:https://dx.doi.org/10.1594/pangaea.54734
https://doi.pangaea.de/10.1594/PANGAEA.54734
Description
Summary: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, ... : Supplement to: Kyle, Philip R (1998): Ferrar dolerite clasts from CRP-1 drillcore. Terra Antartica, 5(3), 611-612 ...