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Philip T. Leat

Researcher at British Antarctic Survey

Publications -  134
Citations -  7369

Philip T. Leat is an academic researcher from British Antarctic Survey. The author has contributed to research in topics: Basalt & Volcanic rock. The author has an hindex of 45, co-authored 131 publications receiving 6790 citations. Previous affiliations of Philip T. Leat include Durham University & Lancaster University.

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Journal ArticleDOI

Geochemistry and tectonic significance of peridotites from the South Sandwich arc-basin system, South Atlantic

TL;DR: Petrographic and geochemical studies of peridotites from the South Sandwich forearc region provide new evidence for the evolution of the south-sandwich arc-basin system and for the nature of interactions between arc magma and oceanic lithosphere as mentioned in this paper.
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The Chon Aike province of Patagonia and related rocks in West Antarctica: A silicic large igneous province

TL;DR: The field occurrence, age, classification and geochemistry of the Mesozoic volcanic rocks of Patagonia and West Antarctica are reviewed, using published and new information in this paper, where a diachronism is recognized between the Early-Middle Jurassic volcanism of eastern Patagonian (Marifil and Chon Aike formations) and the Middle Jurassic-earliest Cretaceous volcanisms of the Andean Cordillera (El Quemado, Ibanez and Tobifera formations).
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Tracing the Indian Ocean Mantle Domain Through Time: Isotopic Results from Old West Indian, East Tethyan, and South Pacific Seafloor

TL;DR: In this article, age-corrected Nd, Pb, and Sr isotopic data for 46-150 Ma seafloor lavas from sites in the western Indian Ocean and ocean-ridge-type Tethyan ophiolites (Masirah, Yarlung-Zangpo) reveal the presence of both Indian-Ocean-type compositions and essentially Pacific-North Atlantic-type signatures.
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Origins of Large Volume Rhyolitic Volcanism in the Antarctic Peninsula and Patagonia by Crustal Melting

TL;DR: In this paper, the origin of V1 and V2 rhyolites from the Antarctic Peninsula using major and trace element and isotopic (Sr, Nd, O) data was evaluated.
Book ChapterDOI

Silicic volcanism: an undervalued component of large igneous provinces and volcanic rifted margins

TL;DR: The role of silicic magmatism in the evolution of a large igneous province and rifted margin may therefore be largely overlooked as discussed by the authors, however, due to the lack of detailed structural features, such as dike swarms, major intrusions, and deeply subsided intracaldera µlls, the role of these volcanic rocks is not fully explored.