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- W1821131952 abstract "The ubiquitous presence of granulites in continental shield areas indicates that high-grade metamorphism has been a fundamental process in the development and stabilisation of Precambrian deep crust. Recent controversy concerning granulite metamorphism and lower crustal processes has focussed, first, upon the large scale tectonic implications of variations in granulite pressure (P)-temperature (T) regimes and pressure-temperature-time paths (P-T-t) and, second, upon definition of the physical and chemical processes responsible for the low water activities generally characteristic of granulites. Whereas some studies have interpreted a general uniformity of P-T conditions and paths for granulites, it has recently been emphasised that granulite terranes display diversity in these features. A spectrum of tectonic models or settings is required to explain, for example, contrasting near-isothermal decompression (ITD) and near-isobaric cooling (IBC) post-peak P-T histories, particularly in the light of structural and geochronological data bearing on the relative timing and timescale of metamorphism." @default.
- W1821131952 created "2016-06-24" @default.
- W1821131952 creator A5013925454 @default.
- W1821131952 date "1992-01-01" @default.
- W1821131952 modified "2023-10-03" @default.
- W1821131952 title "Chapter 8 Proterozoic Granulite Terranes" @default.
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