Provenance and origins of a Late Paleozoic accretionary complex within the Khangai–Khentei belt in the Central Asian Orogenic Belt, central Mongolia

Journal of Asian Earth Sciences(2013)

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Abstract
•Gorkhi Formation clastic rocks were sourced from plutonic rocks in continental margin and continental island arc.•The depositional age of the Gorkhi Formation is 340–320Ma.•Spatial and temporal changes in the provenance of the accretionary complex are proposed.
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Key words
Accretionary complex,Central Asian Orogenic Belt,Carboniferous,Geochemistry,Gorkhi Formation,Sandstone,U–Pb dating,Zircon
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