Geochemical fingerprints of glacially eroded bedrock from West Antarctica: detrital thermochronology, radiogenic isotope systematics and trace element geochemistry in Late Holocene glacial-marine sediments.

Geochemical provenance studies of glacial-marine sediments provide a powerful approach to describe subglacial geology, sediment transport pathways, and past ice sheet dynamics. The marine-based West Antarctic Ice Sheet (WAIS) is considered highly vulnerable to ocean warming and sea level rise that i...

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Bibliographic Details
Published in:Earth-Science Reviews
Main Authors: Simoes Pereira, P, Van de Flierdt, T, Hemming, SR, Hammond, SJ, Kuhn, G, Brachfeld, S, Doherty, C, Hillenbrand, CD
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2018
Subjects:
Online Access:http://hdl.handle.net/10044/1/59340
https://doi.org/10.1016/j.earscirev.2018.04.011