The geological history and evolution of West Antarctica

TA Jordan, TR Riley, CS Siddoway - Nature Reviews Earth & …, 2020 - nature.com
West Antarctica has formed the tectonically active margin between East Antarctica and the
Pacific Ocean for almost half a billion years, where it has recorded a dynamic history of …

Lithological and alteration mineral mapping in poorly exposed lithologies using Landsat-8 and ASTER satellite data: North-eastern Graham Land, Antarctic Peninsula

AB Pour, M Hashim, JK Hong, Y Park - Ore Geology Reviews, 2019 - Elsevier
Antarctica remains a remote and logistically difficult region to conduct geological field
mapping and mineral exploration. Remote sensing satellite imagery has high potential to …

Triassic to Middle Jurassic geodynamic evolution of southwestern Gondwana: From a large flat-slab to mantle plume suction in a rollback subduction setting

C Navarrete, G Gianni, A Encinas, M Márquez… - Earth-science …, 2019 - Elsevier
A novel geodynamic evolution model of the southwestern region of Gondwana from the late
Triassic to the middle Jurassic period is proposed in this contribution, based on new data …

Autochthonous v. accreted terrane development of continental margins: a revised in situ tectonic history of the Antarctic Peninsula

A Burton-Johnson, TR Riley - Journal of the Geological Society, 2015 - lyellcollection.org
The allochthonous terrane accretion model previously proposed for the geological
development of the Antarctic Peninsula continental margin arc is reviewed in light of recent …

A revised interpretation of the Chon Aike magmatic province: active margin origin and implications for the opening of the Weddell Sea

J Bastias, R Spikings, T Riley, A Ulianov, A Grunow… - Lithos, 2021 - Elsevier
Abstract Late Triassic–Jurassic igneous rocks of the Antarctic Peninsula and Patagonia
provide evidence for the evolution of the margin of southwestern Gondwana. We present …

Reconstructions before rifting and drifting reveal the geological connections between Antarctica and its conjugates in Gondwanaland

JJ Veevers - Earth-Science Reviews, 2012 - Elsevier
The initial (200–175Ma) breakup of Pangea was marked by the emplacement of the Large
Igneous Provinces (LIPs) of Karoo–Ferrar-SE Australia (KFS) in the back-arc of …

The geological and tectonic evolution of the Transantarctic Mountains: a review

DH Elliot - Geological Society, London, Special Publications, 2013 - lyellcollection.org
The development of the Transantarctic Mountains was initiated with the rifting of Rodinia and
the formation of a late Neoproterozoic passive continental margin. In Cambrian time this rift …

Dataset compilation by GRASS GIS for thematic mapping of Antarctica: Topographic surface, ice thickness, subglacial bed elevation and sediment thickness

P Lemenkova - Czech Polar Reports, 2021 - papers.ssrn.com
This paper presents the GRASS GIS-based thematic mapping of Antarctica using scripting
approach and associated datasets on topography and geophysics. The state-of-the art in …

Tracking the tempo of a continental margin arc: Insights from a forearc succession in West Antarctica

TR Riley, MJ Flowerdew, A Carter… - Geological …, 2024 - pubs.geoscienceworld.org
The Fossil Bluff Group of eastern Alexander Island records the exceptional preservation of
more than 8 km of Mesozoic sedimentary rocks deposited into an accretionary forearc basin …

a Antarctic Peninsula and South Shetland Islands: volcanology

PT Leat, TR Riley - 2021 - pubs.geoscienceworld.org
The voluminous continental margin volcanic arc of the Antarctic Peninsula is one of the
major tectonic features of West Antarctica. It extends from the Trinity Peninsula and the …