PALAEOGEOTHERMS - IMPLICATIONS OF DISEQUILIBRIUM IN GARNET LHERZOLITE XENOLITHS
MEASURES of the Earth's thermal structure and evolution are important for understanding the driving forces of many geological processes. Estimates of the present variation of temperature with depth in the Earth can be made from surface heat-flow values together with assumptions concerning the c...
| 主要な著者: | , |
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| フォーマット: | Journal article |
| 言語: | English |
| 出版事項: |
1978
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