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The activities of the three large strike-slip fault systems—the Karakoram, the Karakax, and the Longmu Co-Guozha Co faults—located in the western Tibetan Plateau have induced the intense exhumation of the Karakoram and the southern Western Kunlun ranges. However, the histories of these faults remain debated or loosely constrained, partly due to the restricted access to bedrock samples and associated comprehensive analyses. The application of detrital provenance analysis and detrital thermochronology to sediments can provide valuable information on the locations, crystallization timing, and exhumation of the source terranes of the sediments, thereby shedding light on tectonic histories. This study utilizes modern fluvial sand to obtain exhumation information on the Karakoram and the southern Western Kunlun ranges and to reconstruct the history of the major faults. We achieve this through provenance analysis (heavy-mineral analysis and detrital zircon U Pb dating) and detrital apatite fission-track dating. Our results reveal widespread Paleogene rock exhumation across the western Tibetan Plateau and focused mid-Miocene (ca. 15–12 Ma) exhumation along the Karakoram and the southern Western Kunlun ranges. Moreover, the Karakoram Range experienced renewed exhumation at ca. 7 Ma. Through an integration of our results and regional geological evidence, we suggest that the focused mid-Miocene exhumation reflects the initiation of the Karakoram and the Karakax faults; the subsequent ca. 7 Ma exhumation episode of the Karakoram Range indicates a regional kinematic reorganization due to the initiation of the Longmu Co-Guozha Co Fault. We propose that the middle and late Miocene strike-slip faulting in the western Tibetan Plateau was driven by the oblique underthrusting of the Indian lithosphere. • The Karakoram Fault and the Karakax Fault initiated synchronously at ca. 15 Ma. • The Longmu Co-Guozha Co Fault likely initiated at ca. 8–7 Ma. • Oblique underthrusting of Indian slab triggers Miocene strike-slip in western Tibet. [ABSTRACT FROM AUTHOR]

In this article, we report the results of a study on occurrence of a mass-movement event classified as 'rock avalanche' over the North Terong glacier (a tributary of the Siachen Glacier in the Nubra Valley), using multi-date remote-sensing data of Landsat Thematic Mapper (TM), Enhanced Thematic Mapper Plus (ETM+), and Operational Land Imager (OLI) and its effects on glacier-surface velocity. Normalized cross-correlation image matching method for displacement measurements at sub-pixel level using Computer Imaging Analysis Software (CIAS), an add-on module of Environment for Visualizing Images (ENVI) software, was used to map changes in the position of debris-deposits of the rock avalanche and assess variations in glacier-surface velocities. Well-defined debris margins gave positions of debris on different dates. Study indicated that this rock avalanche must have occurred between 21 April 2000 and 8 May 2000 (possibly on 3 or 4 May). It induced a kinematic wave or a 'mini-surge' in the glacier with its surface velocity showing almost twofold increase in post-event period. [ABSTRACT FROM AUTHOR]

[Display omitted] • Heterogeneity in stress field, suggesting non-uniform seismic hazard in the region. • Central Himalaya exhibits arc-normal principal stress, parallel to plate motion. • Western Himalaya displays arc-oblique principal stress right-angles to plate motion. • We suggest the M w 7.6 Kashmir earthquake (2005) to be the Himalayan-type. • Zones with Low stress ratios suggest the role of local and multiple tectonic forces. In this study, we use iterative joint stress inversion technique on a declustered catalogue of 324 focal mechanisms to evaluate the stress distribution in the western India-Eurasia collision zone (IECZ). The stress field has been obtained for different tectonic settings, such as the Himalayan Seismic belt, Karakoram-Tibet region and the individual zones identified based on geology, tectonics and available focal mechanism solutions. The results reveal NE-SW trending principal stress (σ 1) with compression for Himalayan seismic belt and strike-slip stress regime for Karakoram-Tibet. We observe that even within the Himalayan region, the western region (75°-77° E latitudes) exhibits arc-oblique compression (NE-SW) in contrast to the arc-normal compression (NNE-SSW) in central Himalaya beyond 77°E; consistent with GPS vectors. The Stress field for the aftershock sequence of 2005 Kashmir earthquake in the Hazara Syntaxis region displays dissimilarity with its adjoining regions (Pamir, Nanga Parbat, Hindukush, etc.), but exhibits similarity with the Central Himalaya. Within the Karakoram-Tibet region, the Karakoram fault exhibits NNE-SSW oriented principal stress with transpressional fault motion, while the Kaurik Chango rift shows N-S oriented principal stress with transtensional motion. The stress ratio in the western IECZ broadly varies between 0.07 and 0.9, suggesting the prominent role of the intermediate stress axis (σ 2) in the areas of low-stress ratios. The inferences drawn suggest that the stress distribution in the western IECZ is heterogeneous with variable seismic hazard. [ABSTRACT FROM AUTHOR]

Abstract: Determining the slip-rate history along the right-lateral Karakorum fault (KF) is fundamental to understanding its present-day kinematic role in the deformation of Tibet. Geodetic and geologic studies suggest slip-rates of 0–11mm/yr along this structure. Whether slip-rate variability exists along strike and/or time, or simply results from different measuring techniques/timescales, remains unknown. In order to constrain slip-rates within a timescale of 200ka, we studied fluvial and glacial geomorphic features that are right-laterally or vertically offset by the fault by varying amounts from 7±1m to 430±30m and up to 53±5m, respectively. We constrained their ages using 10Be surface exposure dating on 141 quartz-rich samples collected on 4 lateral moraines and at 3 alluvial sites along the southernmost segment of the KF (Menshi–Kailas basin) and along the Gurla Mandhata detachment fault in the Pulan graben. From the 30° fault bend at Baer (80.5°E) to Mount Kailas area, the slip-rate along the KF is >7.1+3.2/−1.7 mm/yr at Menshi and >7.9+3.2/−2.5 mm/yr at Kailas (slip on two parallel fault strands). In the Pulan graben, the normal fault slip-rate is >1.6+0.4/−0.3 mm/yr. Our data suggest that the Quaternary slip-rate along the southern KF does not decrease eastward but is constant along strike for at least 200km, from >5–11mm/yr in the Gar basin further north to >7–8mm/yr in the Menshi–Kailas basin. Because no expected along-strike slip-rate gradient is observed, it implies that the KF does not end at the Kailas but must extend where the slip rate decreases, i.e. eastward along the Yarlung Zangbo suture and southward along the Gurla Mandhata–Humla fault system. [Copyright &y& Elsevier]

Structural style along the active, NW-striking, right-slip Karakoram fault in western Tibet ranges from transpression in the north (37° to 34°N) to transtension in the south (34° to 32°N). This transition in structural style occurs at a 27-km-wide bend in the fault. Our new neotectonic mapping has documented the long-asserted structural linkage between the ENE-striking Gozha–Longmu Co fault system and the similarly oriented active, leftslip Altyn Tagh fault to the northeast. This mapping also indicated that the restraining bend in the Karakoram fault is located where this fault intersects the Gozha-Longmu Co extension of the Altyn Tagh fault to the west. Additional observations from remotely sensed imagery suggest that the total left-separation along the Gozha-Longmu Co fault system is 25-32 km. We use the new neotectonic mapping and published slip rates to develop a simple kinematic model for the main active faults in western Tibet to explore the genetic relationship between slip along the Gozha- Longmu Co fault system and the geometric and kinematic evolution of the Karakoram fault. This model combines published geodetic and Quaternary slip rates with the known fault geometries and demonstrates that the transition from transpression to transtension along the Karakoram fault can be explained by differential motions between the NW Himalaya, the Tianshuihai terrane, and the Tibetan Plateau. These motions produce bending and transtension along the central and southern Karakoram, respectively, and movement of the Tibetan Plateau at a rate of 6–13 mm/ yr toward the east-southeast relative to the Pamirs. We also fi nd that the Gozha–Longmu Co fault system likely initiated between 10 and 3 Ma to accumulate 25–32 km of total left separation. We suggest that the Gozha-Longmu Co fault system formed during late Miocene to Pliocene structural reorganization of the southwestern Altyn Tagh and southern Karakoram fault systems to allow eastward migration of the Tibetan Plateau and northward migration of the Pamir syntaxis. [ABSTRACT FROM AUTHOR]