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- W1437142570 endingPage "410" @default.
- W1437142570 startingPage "357" @default.
- W1437142570 abstract "It is a common perception that high-grade metamorphism typifies rocks of Archean age. While many large granulite complexes are indeed Archean, there also exist many well-preserved low-grade Archean sequences, implying a range of exhumation magnitude and tectonic controls. The abundance of high-grade rocks in regions of Archean age, along with the widespread occurrence of Archean komatiites, taken to indicate hotter mantle conditions, have given rise to speculation that the early Earth was characterized by considerably higher geothermal gradients than today. There is growing recognition that many granulites of Archean and younger age formed in continental marginal settings, along highly perturbed geotherms, and making estimates of geothermal gradient from metamorphic assemblages relevant only to transient conditions." @default.
- W1437142570 created "2016-06-24" @default.
- W1437142570 creator A5039816461 @default.
- W1437142570 date "1994-01-01" @default.
- W1437142570 modified "2023-10-17" @default.
- W1437142570 title "Chapter 9 Archean High-Grade Metamorphism" @default.
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