Anomalously High Heat Flow Regions Beneath the Transantarctic Mountains and Wilkes Subglacial Basin in East Antarctica Inferred From Curie Depth

The Transantarctic Mountains (TAMs) separate the warmer lithosphere of the Cretaceous-Tertiary West Antarctic rift system and the colder and older provinces of East Antarctica. Low velocity zones beneath the TAM imaged in recent seismological studies have been interpreted as warm low-density mantle...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Lowe, M, Mather, B, Green, C, Jordan, TA, Ebbing, J, Larter, R
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://eprints.whiterose.ac.uk/195228/
https://eprints.whiterose.ac.uk/195228/3/JGR%20Solid%20Earth%20-%202022%20-%20Lowe%20-%20Anomalously%20High%20Heat%20Flow%20Regions%20Beneath%20the%20Transantarctic%20Mountains%20and%20Wilkes.pdf
https://doi.org/10.1029/2022jb025423