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- W2349273344 abstract "Detail studies on modern continental margins have demonstrated that tectonic divisions and evolutions only based on ophiolite suits are always elusive. In contrast,analyses of sedimentary buildups may provide positive constrains for identification of tectonic units and then help deduce reasonable tectonic evolutions. Detailed geological mapping with scale of 1∶250000 on the west segment of the southern Kunlun suture demonstrated that the southern Kunlun ophiolite suit represents in fact an infant rather than a mature oceanic crustal slice. The associated sedimentary rocks are mainly continental clastics or carbonates. From the Permian to Triassic and from the north to the south,the stratigraphic buildups are gradually variable from continental clastics to turbidite without any volcanic rocks,suggesting they deposited in a rifted passive continental marginal basin. Its abyssal oceanic basin (the Jinshajiang ocean) was located in south of the Kunlun suture. The Jurassic piggyback foreland basin developing upon the folded Permian to Triassic strata indicated the termination of the Indosinian tectonic event." @default.
- W2349273344 created "2016-06-24" @default.
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- W2349273344 date "2009-01-01" @default.
- W2349273344 modified "2023-09-24" @default.
- W2349273344 title "Late Paleozoic Strata and Tectonic Facies in the Northern Margin of the Eastern Kunlun Orogen and their Tectonic Implications" @default.
- W2349273344 hasPublicationYear "2009" @default.
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