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• W2012326879 abstract "Low-pressure metamorphic facies (i.e. high T/P ratios) are widespread in a wide range of tectonic settings. Explanations offered for the occurrence of these facies include extensional and/or magmatic models. However, these fail to explain that the low-P facies metamorphism is commonly coeval with a phase of pervasive crustal thickening, with T/P ratios increasing during, or slightly lagging behind, the thickening. We propose an alternative explanation based on the approximate synchroneity of crustal thickening and erosion (thinning) of the mantle lithosphere." @default.
• W2012326879 created "2016-06-24" @default.
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• W2012326879 creator A5062506223 @default.
• W2012326879 date "1990-05-01" @default.
• W2012326879 modified "2023-10-11" @default.
• W2012326879 title "A model for low-pressure facies metamorphism during crustal thickening" @default.
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• W2012326879 doi "https://doi.org/10.1111/j.1525-1314.1990.tb00472.x" @default.
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