Results 111 to 120 of about 4,789 (265)

Supplemental Material: Construction of the Lesser Himalayan–Subhimalayan thrust belt: The primary driver of thickening, exhumation, and high elevations in the Himalayan orogen since the middle Miocene

, 2021
Sean P. Long, Delores M. Robinson
openalex   +2 more sources

Mid-Pleistocene climate transition drives net mass loss from rapidly uplifting St. Elias Mountains, Alaska [PDF]

, 2016
Erosion, sediment production and routing on a tectonically active continental margin reflect both tectonic and climatic processes; partitioning the relative importance of these processes remains controversial.
Asahi, H, Bahlburg, H, Bailey, I, Belanger, CL, Berbel, GBB, Childress, L, Cowan, E, Drab, L, Enkelmann, E, Forwick, M, Fukumura, A, Ge, S, Gulick, SPS, Gupta, S, Jaeger, JM, Kioka, A, Konno, S, LeVay, LJ, Maerz, C, Matsuzaki, KM, McClymont, EL, Mix, AC, Moy, C, Mueller, J, Nakamura, A, Ojima, T, Reece, R, Ribeiro, FR, Ridgway, KD, Romero, OE, Slagle, AL, St-Onge, G, Stoner, J, Suto, I, Swartz, JM, Walczak, MD, Worthington, LL   +36 more
core   +1 more source

Supplemental Material: Permian plume-strengthened Tarim lithosphere controls the Cenozoic deformation pattern of the Himalayan-Tibetan orogen [PDF]

, 2020
Xu Xi, Hanlin Chen, et al.
openalex   +2 more sources

Tectono-sedimentary evolution of upper Assam “inter-orogenic” peripheral foreland basin, India

Discover Geoscience
The northern periphery of the Indian craton is the leading edge of the under-thrusting continent in the continent–continent collision set up between the Indian and Eurasian plates.
S. K. Biswas, Gaurav Chauhan
doaj   +1 more source

Out-of-sequence faulting of the Jwalamukhi Thrust, India [PDF]

, 2016
The southernmost thrust of the Himalayan orogenic wedge that separates the foreland from the orogen, the Main Frontal Thrust, is thought to accommodate most of the ongoing crustal shortening in the Sub-Himalaya.
Bookhagen, Bodo, Dey, Saptarshi, Scherler, Dirk, Schildgen, Taylor F., Strecker, Manfred R., Thiede, Rasmus C., Wittmann, Hella   +6 more
core   +1 more source

Tectonics Influence The Climate Change In The Himalayan Orogenic Belt

, 2019
Introduction The high altitude mountain system (i.e., Himalaya) and the Tibetan Plateau region formed after the intracontinental collision of the Indian and Eurasian plates during 55–50 Ma (Neupane et al., 2017 and reference therein). The Himalayan range, separating the plains of the Indian subcontinent from the Tibetan Plateau, extends 2,400 km-long ...
Bhupati Neupane, Junmeng Zhao, Sanjev Dhakal   +2 more
openaire   +1 more source

Kinematics and Vorticity in Kangmar Dome, Southern Tibet: Testing Midcrustal Channel-flow Models for the Himalaya [PDF]

, 2010
Kinematic, kinematic vorticity (Wm), and deformation temperature analyses were completed to test the hypothesis that midcrustal rocks exposed in the core of the Kangmar gneiss dome, southern Tibet record ductile deformation patterns of a “frozen” segment
Hacker, Bradley R., Lee, Jeffrey, Seward, Gareth, Wagner, Tom   +3 more
core   +2 more sources

Supplemental Material: The impact of a tear in the subducted Indian plate on the Miocene geology of the Himalayan-Tibetan orogen

, 2021
Rui Wang, et al.
openalex   +3 more sources

Sedimentological and chemostratigraphic constraints on the provenance of sandstones and mudstones from the Kuldana and Murree formations in the Sub Himalayas

Discover Geoscience
The Kuldana Formation and Murree Formation along the eastern margin of the Hazara Kashmir Syntaxis (HKS) in Pakistan’s sub-Himalayas, particularly in the Haveli district, were studied for their sedimentological, geochemical, and petrographic ...
Khawaja Umair Majeed, Muhammad Saleem Mughal, George Kontakiotis, Muhammad Basharat, Hammad Tariq Janjuhah, Usama Sabir Khokhar, Muhammad Rustam Khan, Evangelia Besiou, Assimina Antonarakou, Tahir Abbas   +9 more
doaj   +1 more source

Uplift, Climate and Biotic Changes at the Eocene-Oligocene Transition in Southeast Tibet [PDF]

, 2018
The uplift history of southeastern Tibet is crucial to understanding processes driving the tectonic evolution of the Tibetan Plateau and surrounding areas.
Deng, Cheng-Long, Deng, Wei-Yu-Dong, Huang, Jian, Huang, Yong-Jiang, Jia, Lin-Bo, Li, Shi-Hu, Li, Shu-Feng, Liu, Jia, Sherlock, Sarah, Spicer, Robert A., Su, Tao, Valdes, Paul J., Wang, Li, Xu, He, Zhang, Shi-Tao, Zhou, Zhe-Kun   +15 more
core   +3 more sources