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Detailed Reference Information |
Berner, U. and Bertrand, P. (1990). Evaluation of the Paleo-geothermal gradient at site 768 (SULU Sea). Geophysical Research Letters 17: doi: 10.1029/90GL02122. issn: 0094-8276. |
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Paleo-temperature gradients for Site 768 are determined by modelling organic maturites. It is found that the measured maturity of the organic matter cannot be attributed to the present-day thermal gradient of 130 ¿C/Km. From a comparison between modelled and measured maturities a high paleo-gradient of 250 ¿C/km is derived. ¿American Geophysical Union 1990 |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Marine Geology and Geophysics, Heat flow (benthic) and hydrothermal processes, Information Related to Geographic Region, Pacific Ocean |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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