THE FLUID REGIME OF HIGH-TEMPERATURE METAMORPHISM DURING GRANITOID MAGMA GENESIS
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dc.contributor.author | Clemens J.D. | |
dc.contributor.author | Watkins J.M. | |
dc.date.accessioned | 2021-03-03T03:56:31Z | |
dc.date.available | 2021-03-03T03:56:31Z | |
dc.date.issued | 2001 | |
dc.identifier | https://elibrary.ru/item.asp?id=13695699 | |
dc.identifier.citation | Contributions to Mineralogy and Petrology, 2001, 140, 5, 600-606 | |
dc.identifier.issn | 0010-7999 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/26191 | |
dc.description.abstract | The strong negative correlation between the temperatures and melt H2O contents of granitoid magmas implies that the crustal melting reactions that produced the magmas were strongly buffered, with T and aH2O co-varying within a narrow band. This observation can only be explained if the partial melting reactions that created the magmas were either fluid-absent from the outset or evolved toward this condition as melting progressed. Since these melting reactions occur during upper amphibolite- to granulite-facies metamorphism, it is reasonable to conclude that metamorphic events responsible for the generation of granitoid magmas generally occur in the absence of excess pervasive fluid. | |
dc.title | THE FLUID REGIME OF HIGH-TEMPERATURE METAMORPHISM DURING GRANITOID MAGMA GENESIS | |
dc.type | Статья |
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