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...
المؤلفون الرئيسيون: | , |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
1984
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