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the early phases with the India–Asia continental collision are missing. The western Tarim Basin on the northeastern margin on the Pamir provides an excellent prospect to analyze their development and evolution.

zone Using the interpretation of seismic profile, though inside the Tiklik thrust zone, without having details to 354

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cross-segment combined with the apatite fission-track success advise that the Hotan-Tiklik phase 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-area of seismic profiles to ascertain the timing and shortening magnitude of the Hotan 148

Stocking Feat thirteen December 2016

activity of the Tiklik fault considering the fact that mid- to late-Miocene is in keeping with the unconformity amongst 451

A Kenai father, two teenage daughters and two good friends set off Friday night by boat for just a weekend at a public use cabin about the north shore of Tustumena Lake. The tour before long became a lot more risky than anybody predicted.

to the structural and apatite fission-monitor leads to this examine. See the text for comprehensive discussions. 823

fault all through these intervals. The later phase corresponded to synchronous activity with the Hotan fault, 401

Hotan fault slips together the detachment layer in the lowermost Paleogene strata and the majority of the slip 365

Results from apatite fission monitor thermochronology together with development strata and well balanced tiklik.com cross section reveal which the Hotan-Tiklik phase underwent two-stage deformation: (one) enhancement from the Tiklik thrust over the late Oligocene-early Miocene and again Because the mid- to late Miocene and (2) action from the Hotan thrust For the reason that mid- to late Miocene on account of basinward propagation of thrusting. The balanced cross section, combined with the apatite fission observe success, suggests that the Hotan-Tiklik segment contributes a total shortening magnitude of a lot more than ca. 34 ± six km. Within just this, ca. four ± two and ca. 23 ± one km of the shortenings were absorbed through the Hotan anticline along with the Hotan detachment fault, respectively, both equally of which were being connected to detachment levels. This implies that detachment levels performed an successful job in propagating deformation within the western Tibetan Plateau into the Tarim Basin.

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