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"The closing of the southern branch of the Paleo-Asian Ocean: Constrain" by Yazhuo Niu, G. R. Shi et al.

The Carboniferous–Permian strata in the southern Beishan Orogenic Collage (BOC) have been regarded as deposits formed either in a branch of the Paleo-Asian Ocean (PAO) or in continental rift basins. This paper presents stratigraphic, sedimentological, and provenance data of a continuous Carboniferous–Permian sequence on the southern margin of the Shuangyingshan Block within the southern BOC in NW China. Carboniferous Baishan and Shibanshan formations record a shallowing-upward change from marine tidal flat to continental braided stream environments. Integrated sandstone modes and U-Pb-Hf data indicate that these formations were fed from an orogenic uplift composed of Precambrian and early Paleozoic rocks of the Shuangyingshan and Dunhuang blocks (ca. 2492, 953, and 439–400 Ma). Latest Carboniferous–Early Permian depositional environments shifted from alluvial fans (Ganquan Formation) to delta-front and prodelta environments in an open marine setting (Shuangbutang and Jushitan f ....

Beishan Orogenic Collage , Paleo Asian Ocean , Shuangyingshan Block , Carboniferous Baishan , Latest Carboniferous , Early Permian , Ganquan Formation , Arboniferous Permian , Paleo Asian Ocean , Edimentary Environments , பேலியோ ஆசிய கடல் , ஆரம்ப பெர்மியன் ,