A Geothermal Heat Flux Map of Antarctica Empirically Constrained by Seismic Structure

Author:

Shen Weisen1ORCID,Wiens Douglas A.2ORCID,Lloyd Andrew J.23ORCID,Nyblade Andrew A.4ORCID

Affiliation:

1. Department of Geosciences State University of New York at Stony Brook Stony Brook NY USA

2. Department of Earth and Planetary Sciences Washington University in St Louis St. Louis MO USA

3. Now at Lamont‐Doherty Earth Observatory Columbia University New York NY USA

4. Department of Geosciences Pennsylvania State University University Park PA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference47 articles.

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

2. Spatially Variable Geothermal Heat Flux in West Antarctica: Evidence and Implications

3. Blackwell D. Richards M. Frone Z. Batir J. Ruzo A. Dingwall R.&Williams M. 2011.Temperature‐at‐depth maps for the conterminous US and geothermal resource estimates(no. GRC1029452). Southern Methodist University Geothermal Laboratory Dallas TX (United States).

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

5. Hot rocks in a cold place: high sub-glacial heat flow in East Antarctica

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