High heat flow anomalies over salt structures on the Texas continental slope, Gulf of Mexico

Details High heat flow anomalies over salt structures on the Texas continental slope, Gulf of Mexico High heat flow anomalies over salt structures on the Texas continental slope, Gulf of Mexico

Aug 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19.1687n&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 19, no. 16, Aug. 21, 1992, p. 1687-1690. Research supported by Texas Advance

Other

3

Geothermal Anomalies, Gulf Of Mexico, Heat Transmission, Ocean Bottom, Salt Beds, Conductive Heat Transfer, Sedimentary Rocks

Scientific paper

A series of 74 closely spaced (less than 2 km apart) heat flow measurements were made over two salt structures on the Texas continental slope, Gulf of Mexico. An analysis of the measurement data indicates that a conductive heat flow anomaly can be distinguished under certain conditions if sufficiently detailed measurements are taken. It is demonstrated that heat flow observations can be useful in constraining the geometry of salt bodies.

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