Title Basement controls on deformation during oblique convergence: Transpressive structures in the western Qaidam Basin, northern Tibetan Plateau
Authors Liu, Runchao
Allen, M. B.
Zhang, Qiquan
Du, Wei
Cheng, Xiang
Holdsworth, R. E.
Guo, Zhaojie
Affiliation Peking Univ, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Sch Earth & Space Sci, Beijing 100871, Peoples R China.
Univ Durham, Dept Earth Sci, Elvet Hill, Durham DH1 3LE, England.
Petrochina, Qinghai Oilfield Co, Dunhuang 736202, Gansu, Peoples R China.
Keywords ALTYN-TAGH FAULT
CENOZOIC TECTONIC EVOLUTION
NW CHINA
MAGNETIC-SUSCEPTIBILITY
CONTINENTAL DEFORMATION
NORTHEASTWARD GROWTH
ACTIVE DEFORMATION
ELASTIC THICKNESS
NORTHWEST CHINA
HEXI CORRIDOR
Issue Date 2017
Publisher LITHOSPHERE
Citation LITHOSPHERE.2017,9(4),583-594.
Abstract The Qaidam Basin, especially its western part, is characterized by numerous northwest-trending folds and faults. Understanding the style and formation mechanism of these structures is crucial for unravelling the deformation of the Qaidam Basin and the broader tectonics of the northern part of the Tibetan Plateau. Based on seismic data, we reconstruct the structural framework of the central part of the western Qaidam Basin, and find that: (1) the structures in this area display positive flower geometries in two-dimensional (2D) seismic profiles and helicoidal shapes in 3D space; (2) these positive flower structures began to develop during the middle to late Miocene (15-8 Ma); and (3) these positive flower structures are controlled by left-lateral basement faults and formed in a random temporal sequence. The left-lateral features represent the strike-slip component of distributed deformation, consistent with published global positioning system and seismicity data for oblique convergence across the north of the Tibetan Plateau. Collectively, they perform the same role as the discrete Haiyuan, Kunlun, and Altyn Tagh faults in adjacent areas.
URI http://hdl.handle.net/20.500.11897/471723
ISSN 1941-8264
DOI 10.1130/L634.1
Indexed SCI(E)
Appears in Collections: 地球与空间科学学院
造山带与地壳演化教育部重点实验室

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