CONTINENTAL THERMAL AND TECTONIC REGIMES DURING THE ARCHEAN
Describes how metamorphic pressures estimated from mineral assemblages in Archaean high-grade terrains may be used to constrain geothermal regimes in the Archaean continental crust. Discusses results, which imply that Archaean continental thermal regimes were similar to present-day ones. These obser...
| Prif Awduron: | , |
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| Fformat: | Journal article |
| Iaith: | English |
| Cyhoeddwyd: |
1984
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