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interpretation types amongst their and this scientific tests. Within our model, the hanging wall block with the 364

Oligocene-early Miocene, suggesting a depth level previously above the detachment layer along the 404

U-Pb and Hf isotopic from your east section of Tiekelike tectonic belt: constrains around the timing 682

cross-portion combined with the apatite fission-track final results suggest which the Hotan-Tiklik segment 34

Cette nouvelle économie à donner naissance à plusieurs acteurs dans ce secteur et notamment des nouvelles plateformes en ligne permettant de moderniser le secteur.

cross-portion of seismic profiles to ascertain the timing and shortening magnitude of the Hotan 148

interpreted to mark thrusting and exhumation of the surrounding orogens throughout the Tarim Basin 461

The western Kunlun thrust belt defines the boundary among the stable Tarim Basin in the north and the intensely deformed Cenozoic Tibetan Plateau during the south. Thanks to its vital tectonic situation, comprehension its tectonic evolution should have essential implications for propagation of deformation from Tibet to its neighboring cratonal locations through India-Eurasia convergence. We listed here present new structural analyses based on industry investigations and seismic reflection profiles over the Hotan-Tiklik segment with the western Kunlun thrust belt. The outcome point out the structural section crosses two big thrust zones: the Tiklik zone inside the hinterland to the south as well as Hotan zone while in the foreland towards the north.In just these, the Hotan thrust zone is skinny skinned, with its deformation characterised by fault-bend folding and fault slipping alongside detachment levels, While the Tiklik thrust zone involves basement, with its deformation driven by the at the moment steeply dipping Tiklik fault.

A Kenai father, two teenage daughters and two mates established off Friday evening by boat for any weekend in a general public use cabin on the north shore of Tustumena Lake. The excursion quickly grew to become a great deal more dangerous than anybody predicted.

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amongst the somewhat steady Tarim Basin while in the north along with the intensely deformed western Tibetan fifty one

The Udelhovens are a longtime Kenai household. They often recreate about the lake and are very well accustomed to it, the officers reported.

Cenozoic tectonic rotations in different areas of the NE Pamir: implications with the evolution in the arcuate orogen

The refuge features Tustumena Lake, which is more than 25 miles long and 6 miles large. Its reputation as perilous to small craft occurs with the intense winds that blow down Tustumena Glacier and kick up massive waves in the heartbeat, refuge legislation enforcement officers say.

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