Two types of the crust-mantle interaction in continental subduction zones

Science China-earth Sciences, 2015.

Cited by: 17|Bibtex|Views8|Links

Abstract:

Plate subduction is an important mechanism for exchanging the mass and energy between the mantle and the crust, and the igneous rocks in subduction zones are the important carriers for studying the recycling of crustal materials and the crust-mantle interaction. This study presents a review of geochronology and geochemistry for postcollis...More

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