scholarly journals Correction to “Geology of the Haiyuan Fault Zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the northeastern margin of the Tibetan Plateau”

Tectonics ◽  
1992 ◽  
Vol 11 (1) ◽  
pp. 175-175
Author(s):  
B. C. Burchfiel
Keyword(s):  
Tibetan Plateau ◽  
Fault Zone ◽  
The Tibetan Plateau ◽  
Autonomous Region ◽  
Ningxia Hui Autonomous Region

Geology of the Haiyuan Fault Zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the Northeastern Margin of the Tibetan Plateau

Tectonics ◽  
1991 ◽  
Vol 10 (6) ◽  
pp. 1091-1110 ◽  
Author(s):  
B. C. Burchfiel ◽  
Peizhen Zhang ◽  
Yipeng Wang ◽  
Weiqi Zhang ◽  
Fangmin Song ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Fault Zone ◽  
The Tibetan Plateau ◽  
Autonomous Region ◽  
Ningxia Hui Autonomous Region

scholarly journals Lhasa seismicity during 2004-2006

2008 ◽  
Vol 38 ◽  
pp. 9-14
Author(s):  
Tsoja Wangmo ◽  
Norsang Gelsor ◽  
Jens Havskov ◽  
Nima Puntsog ◽  
Baima Tsering
Keyword(s):  
Tibetan Plateau ◽  
Active Region ◽  
Fault Zone ◽  
Seismic Activity ◽  
Measured Data ◽  
Seismic Network ◽  
The Tibetan Plateau ◽  
Seismic Region ◽  
Set Up

The Tibetan Plateau is an active seismic region due to the collision between Indian and Eurasian plates. We have set up a new seismic network in the heart of the Tibetan Plateau, in the Lhasa region, to detect seismic activities. The measured data show that Lhasa is a seismically active region where at least 716 earthquakes were detected and a total of 218 events of magnitude greater than 2.0 occurred in the period between January 2004 and July 2006. Out of them, 11 earthquakes had a magnitude greater than 5.0. A high seismic activity was observed along the Dangshung fault zone.

Huge Landslides along the Jinsha River in Southeastern Tibetan Plateau and Their Association with the Recent Activity of Jinsha River Fault Zone

2020 ◽  
Author(s):  
Zufeng Chang ◽  
Hao Chang ◽  
Zebin Mao ◽  
Ruojin Guo
Keyword(s):  
Tibetan Plateau ◽  
Fault Zone ◽  
Large Scale ◽  
Late Quaternary ◽  
Average Rate ◽  
Economic Losses ◽  
The Tibetan Plateau ◽  
Jinsha River ◽  
Water Storage Capacity ◽  
Barrier Lake

<p>     The Jinsha river fault zone in the eastern margin of the Tibetan Plateau is an old suture structure after the shutting of the proto-Tethys and a large scale ultra-lithosphere fault zone consisted of  5 to 6 fault branches with a width of 50km, have a long  geological evolution history. Since late Quatery, this fault zone is mainly dominated by dextral strike slip with partial thrusting component, absorbing  partial energy of the extrusion movement of  Tibetan Plateau. Along the fault zone, lower terraces of Jinsha river at Muronglou, Buzhong, Langzhong, Guxue, etc. were displaced, indicating the fault zone is active in late Quaternary, with an average rate of 3.5～4.3mm/ /yr. horizontally and 0.9-1.1mm/yr. vertically respectively in Holocene. Influenced by the intense fault activity of Jinsha river fault zone, this region is characterized by fractured rocks, strongly weathered surfaces.</p><p>      The Jinsha river, the upstream of the Yangtze river, parallel to Jinshajiang fault zone, flows from north to south, forming deep river valley and huge terrain elevation difference. Numerous huge landslides have developed along the river, for example, there are 23 giant avalanches in the 38 km long reach from Narong to Rongxue, with general volumes of 10~70 million m<sup>3</sup> and even up to several hundreds million m<sup>3</sup>. Moreover, the landslides produce many loose clastic fragments which detonate many debris flows and river blocking. The latest disaster event is the Baige barrier lake in 2018 caused by landslide, with a water storage capacity of 524 million m<sup>3</sup>, causing tens of billions of yuan of economic losses. These landslides are distributed along the fault and its two sides, suggesting that these huge avalanches are closely related to the intense activity of the fault zone and special topography.</p><p>Keywords: Huge landslide, Jinsha River, Jinsha River Fault Zone, late Quatery activity</p>

Characteristics and implications of the stress state in the Longmen Shan fault zone, eastern margin of the Tibetan Plateau

2015 ◽  
Vol 656 ◽  
pp. 1-19 ◽  
Author(s):  
Wen Meng ◽  
Qunce Chen ◽  
Zhen Zhao ◽  
Manlu Wu ◽  
Xianghui Qin ◽  
...  
Keyword(s):  
Stress State ◽  
Tibetan Plateau ◽  
Fault Zone ◽  
The Tibetan Plateau ◽  
Eastern Margin ◽  
Longmen Shan Fault

scholarly journals Near-field motion of the Haiyuan fault zone in the northeastern margin of the Tibetan plateau derived from InSAR permanent scatterers analysis

2013 ◽  
Vol 7 (1) ◽  
pp. 073507 ◽  
Author(s):  
Chunyan Qu ◽  
Xinjian Shan ◽  
Xiaobo Xu ◽  
Guohong Zhang ◽  
Xiaogang Song ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Fault Zone ◽  
Near Field ◽  
The Tibetan Plateau ◽  
Permanent Scatterers
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