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overlying late Paleozoic strata are verified by both equally outcrops and borehole details. Within just 120

portion lengths, fault slip and shortening magnitudes in unique phase. The strata symbols are definitely the 813

Therefore, The expansion strata produced over the Hotan fold present constraints to evaluate the 334

Although syntectonic sedimentation has long been proven to generally be among The key elements linked to thrust belt deformation, earlier scientific tests have mostly focused on the influence of just one stage In this particular context. Two geometric sediment offers which have been referred to as progradation and aggradation are recognized to result in distinctive thrust belt deformation subsequences, but the affect of multistage sedimentary strata stays considerably less perfectly-recognized. Interpretation of the most up-to-date seismic data reveals that the Western Kunlun thrust belt is characterized by classical triangle zone. There are two adjacent sections with distinct geometrical features, a prograding monocline as well as a spaced-ramp anticline. We restored both of these sections and analyzed the probable geological things bringing about their development In this particular review.

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The structural Investigation in the seismic profile indicates that The expansion strata began to develop 338

We also doc exhumation of your shear zone from two low-temperature thermochronologic transects. New apatite (U-Th)/He data and published thermochronologic results reveal two accelerated cooling episodes, backed by stratigraphic and geomorphic observations. The initial speedy cooling stage occurred from ca. 27 to seventeen Ma with elimination of cover rocks and exhumation of the shear zone. The tiklik.com next accelerated cooling episode discovered by our AHe facts commenced at fourteen-13 Ma, Long lasting two-3 Myr. The Ailao Shan variety may have risen to its fashionable elevation with significant-relief topography creating because of river incision. We interpret the onset of the speedy exhumation to reflect renewed plateau expansion connected to decreased crustal circulation.

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event could mark the underthrusting from the Tarim block beneath the western Tibetan Plateau, although 494

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As famous higher than, in light on the Hotan thrust zone, the interpretation of seismic profile and its 357

Cenozoic fold and thrust belt in eastern area with the piedmount of west Kunlun and its taper wedge mechanics

Maigaiti slope is sort of 200 km in size, but it really hasn't clear deformation, and taper wedge angle of the fold and thrust belt is fewer than Individuals Energetic orogenies, it's implies the gypsum-mudstone of Aertashi Development and The form of Cenozoic deposition are key aspects, the gypsum-mudstone controls α of taper wedge, the designs of basement and dispositive wedge Regulate β of taper wedge.

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