Analysis of tectonic subsidence and heat flow in the Malay Basin (offshore Peninsular Malaysia)
The Malay Basin has a very high present-day surface heat flow, with an estimated heat flow anomaly of about 33-42 mWm⁻². The heat flow anomaly is interpreted as the result of thinning of the lithosphere during basin formation. The basin is relatively young age (about 35 Ma), which implies that the t...
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| Hlavní autor: | |
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| Médium: | Článek |
| Jazyk: | English |
| Vydáno: |
Geological Society of Malaysia
1997
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| On-line přístup: | http://myagric.upm.edu.my/id/eprint/22513/1/702001-100867-PDF.pdf |
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