Proto-Pacific-margin source for the Ordovician turbidite submarine fan, Lachlan Orogen, southeast Australia: Geochemical constraints
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文摘

Geochemistry of sediments in the Adaminaby Group, Lachlan Orogen suggests a felsic source with continental arc signature.

Granodiorites with a calc-alkaline, shoshonitic signature provided most detritus.

Collisional and continental volcanic arc tectonic settings existed at time erosion of source area took place.

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