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- W4313467569 abstract "Abstract Understanding the three‐dimensional structure, segmentation, and kinematics of complex fault systems is essential to assessing the size of potential earthquakes and related seismic hazards. The Danghe Nan Shan thrust, a major splay of the Altyn Tagh fault (ATF) in north Tibet, is one of these complex fault junctions. Near the town of Subei, the western Danghe Nan Shan thrust composes two left‐stepping faults outlined by fault scarps in front of folded and uplifted alluvial fans and terraces. Age constraints and 2D reconstructions of the accumulated slip above a transient base level of four terraces standing 7–60 m above the present stream bed yield shortening and vertical uplift rates of 0.5 ± 0.1 and 1.1 ± 0.3 mm/yr, respectively, over the last 130 ka on the southern thrust. Along the northern thrust, vertical terrace offsets of 1.5–3.6 m and horizontal slip of 4.5 m documented in a paleoseismological trench occurred after 12 ± 4 ka, constraining coeval rates of 0.3 ± 0.1 mm/yr for uplift and shortening. Overall, 1.4 ± 0.4 mm/yr terrace uplift and 0.8 ± 0.2 mm/yr shortening rates are determined, in agreement with late Miocene long‐term exhumation rate estimates. Our fault mapping and geomorphic and structural observations imply that the western Danghe Nan Shan thrust accommodates slip transfer from the ATF to the west to thrusting and shortening farther east in the Qilian Shan region. Considering the scarp sizes, their lateral extent, the geometry of the faults at depth, and their slip‐rate, we suggest the possible occurrence of Mw 7+ earthquakes near Subei." @default.
- W4313467569 created "2023-01-06" @default.
- W4313467569 creator A5013576381 @default.
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- W4313467569 creator A5042758229 @default.
- W4313467569 creator A5046063756 @default.
- W4313467569 creator A5076801105 @default.
- W4313467569 creator A5089321383 @default.
- W4313467569 date "2022-12-28" @default.
- W4313467569 modified "2023-10-14" @default.
- W4313467569 title "Shortening Rates and Recurrence of Large Earthquakes From Folded and Uplifted Terraces in the Western Danghe Nan Shan Foreland, North Tibet" @default.
- W4313467569 cites W1601348045 @default.
- W4313467569 cites W1626874512 @default.
- W4313467569 cites W1920894272 @default.
- W4313467569 cites W1946046604 @default.
- W4313467569 cites W1964077423 @default.
- W4313467569 cites W1969157568 @default.
- W4313467569 cites W1971152157 @default.
- W4313467569 cites W1972694007 @default.
- W4313467569 cites W1972705099 @default.
- W4313467569 cites W1973858918 @default.
- W4313467569 cites W1975350041 @default.
- W4313467569 cites W1979526534 @default.
- W4313467569 cites W1986047667 @default.
- W4313467569 cites W1995076827 @default.
- W4313467569 cites W1996923801 @default.
- W4313467569 cites W1996948148 @default.
- W4313467569 cites W1997667374 @default.
- W4313467569 cites W1999730394 @default.
- W4313467569 cites W2000936451 @default.
- W4313467569 cites W2002298668 @default.
- W4313467569 cites W2002473398 @default.
- W4313467569 cites W2005035365 @default.
- W4313467569 cites W2008622484 @default.
- W4313467569 cites W2008834035 @default.
- W4313467569 cites W2009425598 @default.
- W4313467569 cites W2010455802 @default.
- W4313467569 cites W2018502726 @default.
- W4313467569 cites W2021927142 @default.
- W4313467569 cites W2023828447 @default.
- W4313467569 cites W2024945077 @default.
- W4313467569 cites W20277813 @default.
- W4313467569 cites W2041191706 @default.
- W4313467569 cites W2041774199 @default.
- W4313467569 cites W2043900361 @default.
- W4313467569 cites W2045701784 @default.
- W4313467569 cites W2046724804 @default.
- W4313467569 cites W2047661207 @default.
- W4313467569 cites W2061678478 @default.
- W4313467569 cites W2063156102 @default.
- W4313467569 cites W2065327555 @default.
- W4313467569 cites W2077048181 @default.
- W4313467569 cites W2079335235 @default.
- W4313467569 cites W2085364474 @default.
- W4313467569 cites W2088331957 @default.
- W4313467569 cites W2092409524 @default.
- W4313467569 cites W2095194310 @default.
- W4313467569 cites W2101333943 @default.
- W4313467569 cites W2102402389 @default.
- W4313467569 cites W2103414293 @default.
- W4313467569 cites W2109267245 @default.
- W4313467569 cites W2119117154 @default.
- W4313467569 cites W2119582894 @default.
- W4313467569 cites W2127150969 @default.
- W4313467569 cites W2127335932 @default.
- W4313467569 cites W2136338903 @default.
- W4313467569 cites W2140709557 @default.
- W4313467569 cites W2140926063 @default.
- W4313467569 cites W2145693114 @default.
- W4313467569 cites W2148162674 @default.
- W4313467569 cites W2151285347 @default.
- W4313467569 cites W2151802599 @default.
- W4313467569 cites W2152546160 @default.
- W4313467569 cites W2166854974 @default.
- W4313467569 cites W2168311633 @default.
- W4313467569 cites W2180911899 @default.
- W4313467569 cites W2208094795 @default.
- W4313467569 cites W2314299591 @default.
- W4313467569 cites W2338890318 @default.
- W4313467569 cites W2347160697 @default.
- W4313467569 cites W2462814450 @default.
- W4313467569 cites W2605534512 @default.
- W4313467569 cites W2609661024 @default.
- W4313467569 cites W2610406133 @default.
- W4313467569 cites W2611588676 @default.
- W4313467569 cites W2766666552 @default.
- W4313467569 cites W2771377455 @default.
- W4313467569 cites W2773981767 @default.
- W4313467569 cites W2782110295 @default.
- W4313467569 cites W2804584889 @default.
- W4313467569 cites W2910769636 @default.
- W4313467569 cites W2914033891 @default.
- W4313467569 cites W2914597267 @default.
- W4313467569 cites W2943039813 @default.
- W4313467569 cites W2954477309 @default.
- W4313467569 cites W2964406276 @default.
- W4313467569 cites W2969766201 @default.
- W4313467569 cites W2980478851 @default.
- W4313467569 cites W2994691442 @default.