Mechanisms to generate ultrahigh-temperature metamorphism

Author:

Jiao ShujuanORCID,Brown MichaelORCID,Mitchell Ross N.ORCID,Chowdhury PriyadarshiORCID,Clark Chris,Chen LinORCID,Chen YiORCID,Korhonen Fawna,Huang GuangyuORCID,Guo Jinghui

Publisher

Springer Science and Business Media LLC

Subject

Nature and Landscape Conservation,Atmospheric Science,Earth-Surface Processes,Pollution

Reference230 articles.

1. Harley, S. L. in Geology Society Special Publications Vol. 138 (eds Treloar, P. J. & O’Brien, P. J.) 81–107 (Geological Society of London, 1998). This article defined UHT metamorphism and recognized two types of post-peak pressure–temperature (P–T) path, which are close to isobaric cooling and close to isothermal decompression.

2. Brown, M. Metamorphic conditions in orogenic belts: a record of secular change. Int. Geol. Rev. 49, 193–234 (2007). This was one of the first articles to document the secular change of metamorphism through Earth history, argue that the occurrence of UHT metamorphism is closely related to the supercontinent cycle and propose the generation of UHT metamorphism in backarc settings.

3. Harley, S. L. Refining the P–T records of UHT crustal metamorphism. J. Metamorph. Geol. 26, 125–154 (2008).

4. Kelsey, D. E. & Hand, M. On ultrahigh temperature crustal metamorphism: phase equilibria, trace element thermometry, bulk composition, heat sources, timescales and tectonic settings. Geosci. Front. 6, 311–356 (2015). This paper provided a systematic review of UHT metamorphism, summarizing major advances including the quantification of UHT conditions by phase equilibrium modelling and trace element thermometry, linking metamorphic ages with P–T points/paths by using HREE partitioning, and providing insight into the heat sources and tectonic settings.

5. White, R. W. & Powell, R. Melt loss and the preservation of granulite facies mineral assemblages. J. Metamorph. Geol. 20, 621–632 (2002).

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