Item talk:Q246125

From geokb

{

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   "name": "Tectonic setting of Cretaceous basins on the NE Tibetan Plateau: Insights from the Jungong basin",
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   "abstract": "Quantifying the Cenozoic growth of high topography in the Indo\u2010Asian collision zone remains challenging, due in part to significant shortening that occurred within Eurasia before collision. A growing body of evidence suggests that regions far removed from the suture zone experienced deformation before and during the early phases of Himalayan orogenesis. In the present\u2010day north\u2010eastern Tibetan Plateau, widespread deposits of Cretaceous sediment attest to significant basin formation; however, the tectonic setting of these basins remains enigmatic. We present a study of a regionally extensive network of sedimentary basins that are spatially associated with a system of SE\u2010vergent thrust faults and are now exposed in the high ranges of the north\u2010eastern corner of the Tibetan Plateau. We focus on a particularly well\u2010exposed basin, located \u223c20\u2003km north of the Kunlun fault in the Anyemaqen Shan. The basin is filled by \u223c900\u2003m of alluvial sediments that become finer\u2010grained away from the basin\u2010bounding fault. Additionally, beds in the proximal footwall of the basin\u2010bounding fault exhibit progressive, up\u2010section shallowing and several intraformational unconformities which can be traced into correlative conformities in the distal part of the basin. The observations show sediment accumulated in the basin during fault motion. Regional constraints on the timing of sediment deposition are provided by both fossil assemblages from the Early Cretaceous, and by K\u2013Ar dating of volcanic rocks that floor and cross\u2010cut sedimentary fill. We argue that during the Cretaceous, the interior NE Tibetan Plateau experienced NW\u2013SE contractional deformation similar to that documented throughout the Qinling\u2013Dabie orogen to the east. The Songpan\u2010Ganzi terrane apparently marked the southern limit of this deformation, such that it may have been a relatively rigid block in the Tibetan lithosphere, separating regions experiencing deformation north of the convergent Tethyan margin from regions deforming inboard of the east Asian margin.",
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