Transpression and transtension zones

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Formation of new continental crust in Western British Columbia during transpression and transtension

Crustal growth in the Coast Mountains, along the leading edge of the Canadian Cordillera, was the result of processes associated with horizontal flow of material during transpression and subsequent transtension, and the vertical accretion of mantle derived melts. From 85 to 58 Ma, as exotic terranes were translated northward during transpression, the crust was thickened to about 55 km, and melt...

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ژورنال

عنوان ژورنال: Geological Society, London, Special Publications

سال: 1998

ISSN: 0305-8719,2041-4927

DOI: 10.1144/gsl.sp.1998.135.01.01