Exhumation of (ultra-)high-pressure terranes: concepts and mechanisms

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Exhumation of (ultra-)high-pressure terranes: concepts and mechanisms

The formation and exhumation of high and ultrahigh-pressure, (U)HP, rocks of crustal origin appears to be ubiquitous during Phanerozoic plate subduction and continental collision events. Exhumation of (U)HP material has been shown in some orogens to have occurred only once, during a single short-lived event; in other cases exhumation appears to have occurred multiple discrete times or during a ...

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ژورنال

عنوان ژورنال: Solid Earth

سال: 2013

ISSN: 1869-9529

DOI: 10.5194/se-4-75-2013