A new heat flux model for the Antarctic Peninsula incorporating spatially variable upper crustal radiogenic heat production-Reference-Cited by-同舟云学术

A new heat flux model for the Antarctic Peninsula incorporating spatially variable upper crustal radiogenic heat production

Published:2017-06-12 Issue:11 Volume:44 Page:5436-5446
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Burton‐Johnson A.¹^ORCID,Halpin J. A.²^ORCID,Whittaker J. M.²^ORCID,Graham F. S.²^ORCID,Watson S. J.²^ORCID

Affiliation:

1. British Antarctic Survey Cambridge UK

2. Institute for Marine and Antarctic Studies University of Tasmania Hobart Tasmania Australia

Funder

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073596

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3. Amante C. andB. W.Eakins(2009) ETOPO1 arc‐minute global relief model: Procedures data sources and analysis National Oceanic and Atmospheric Administration Technical Memorandum NESDIS NGDC‐24.

4. Temperature, lithosphere‐asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities

5. The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurrasic) in the Beardmore Glacier area, Antarctica

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