Hot orogens, tectonic switching, and creation of continental crust: Comment and Reply | Zendy

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Hot orogens, tectonic switching, and creation of continental crust: Comment and Reply

Author(s) -

Michael Brown

Publication year - 2003

Publication title -

geology

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 2.609

H-Index - 215

eISSN - 1943-2682

pISSN - 0091-7613

DOI - 10.1130/0091-7613-31.1.e9

Subject(s) - geology , continental crust , assertion , granulite , tectonics , crust , terrain , continental collision , earth science , collision , geochemistry , paleontology , lithosphere , cartography , geography , facies , computer security , structural basin , computer science , programming language

In a stimulating paper, [Collins (2002][1], p. 535) asserted that “many granulite terrains were too hot to have formed during continental collision” in spite of evidence to the contrary (e.g., [Harley, 1989][2]; [O'Brien and Rotzler, 2003][3]). Based on this assertion, [Collins (2002][1], p.

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