Zobrazeno 1 - 10
of 2 883
pro vyhledávání: '"southern Tibet"'
Publikováno v:
地震科学进展, Vol 54, Iss 10, Pp 649-660 (2024)
The Horba-Tsam Tso rift is one of the major rift systems in southern Tibet, with a general strike of N20°E and a total length of about 200 km, containing 20 parallel or oblique secondary fault zones and graben-half graben systems. The active faults
Externí odkaz:
https://doaj.org/article/b89c5a760a7c49acb081f52bab3c4fed
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 19, Pp n/a-n/a (2024)
Abstract In this study, we utilize C‐band Sentinel‐1 radar images from 2015 to 2022, combined with interseismic horizontal GNSS velocities, to construct large‐scale, high‐resolution, 3‐D velocity and strain rate maps over a vast region of s
Externí odkaz:
https://doaj.org/article/063932bc462e462184031f7d9ddb01c8
Publikováno v:
Applied Sciences, Vol 14, Iss 18, p 8435 (2024)
Amphibole is an important mineral during the differentiation of arc magmas but rarely as a phenocryst in arc lavas or eruptive pyroclastic rocks. The Sanggeda complex, intruded into the ophiolite of the Indus–Yarlung Zangbo Suture Zone (IYZSZ), Zed
Externí odkaz:
https://doaj.org/article/64ecb42ef82d460cb2a00cbac2ae7f93
Autor:
Ming Cheng, Xuming Hu, Yao Tang, Zhao Deng, Yingzi Min, Shiyi Chen, Saijun Sun, Huanzhan Zhou
Publikováno v:
Minerals, Vol 14, Iss 8, p 845 (2024)
The Zhegu area in southern Tibet is situated in the central and eastern part of the Tethys Himalayan tectonic belt, with the Kangbuzhenri area being abundant in gneissic granites. This study examines the petrology, chronology, and geochemistry of the
Externí odkaz:
https://doaj.org/article/3300c54cca6f4ad89fc5850136a699d0
Publikováno v:
Dizhi lixue xuebao, Vol 29, Iss 2, Pp 276-289 (2023)
Sinters in the rift valleys of southern Tibet, including silica sinter and travertine deposits, are the products of hydrothermal activity under regional tectonic movement. Their formation age is significant for studying hydrothermal activity history
Externí odkaz:
https://doaj.org/article/52bfa4da06e74b6d82e3bf49481887f5
Autor:
Bo Xiang, Xiao Xu, Jiahao Yu, Xiaoyu Guo, You Wu, Chunsen Li, Jiajie Wu, Xiaofei Tong, Xucong Luo
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The north-south striking landform perpendicular to the dominant collision zone between the Indian and Eurasian plates was constructed in east-southern Tibet (EST) during the Late Miocene. The building processes remain ambiguous, partly owing to the l
Externí odkaz:
https://doaj.org/article/4e1a13044ae34751b8cac2540e8be659
Autor:
Yanxue Xie, Yildirim Dilek
Publikováno v:
Geosystems and Geoenvironment, Vol 2, Iss 3, Pp 100178- (2023)
We present new U-Pb detrital zircon ages, depositional history and tectonic model for the Liuqu Conglomerate (LQC) in southern Tibet that represents a critical geochronometer for the collision history of the Tibetan-Himalayan Orogenic Belt. LQC is a
Externí odkaz:
https://doaj.org/article/7e4005b86cba4105b2c3f3155626f8c0
Publikováno v:
Minerals, Vol 14, Iss 2, p 141 (2024)
Orogenic antimony-gold deposits contribute significantly to the global antimony resource base. China’s orogenic antimony-gold deposits are primarily in southern Tibet. Investigations indicate that antimony combines and migrates with sulfur hydroxid
Externí odkaz:
https://doaj.org/article/bd4a6c87db1d4476b3a2ff1831105310
Publikováno v:
Minerals, Vol 14, Iss 1, p 66 (2024)
The east–west-trending South Tibetan Detachment System (STDS) and north–south-trending rifts (NSTRs) are the two main types of extensional structures that have developed within the Tibetan Plateau during continent–continent collision since the
Externí odkaz:
https://doaj.org/article/b7d896c3bc764bef8345432e1c34deb1
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