The nature of orogenic lithospheric mantle: Geochemical constraints from postcollisional mafic-ultramafic rocks in the Dabie orogen
Chemical Geology, Volume 334, Issue null, 2012, Pages 99-121.
Continental subduction channelMafic-ultramafic rocksOrogenic lithospheric mantlePostcollisional magmatismSlab-mantle interaction
Postcollisional mafic-ultramafic rocks from the Dabie orogen were studied for their whole-rock major-trace elements and Sr-Nd-Pb isotopes in addition to zircon U-Pb ages and Lu-Hf isotopes. The results provide insights into the nature of orogenic lithospheric mantle in the continental collision zone. The zircon U-Pb dating gave consistent...More
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