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(1976)
Geologic Map of the People's Republic of China (1:4,000,000)
Q.S. Zhang (1980)
Metamorphic geology of the Eastern Qinling Range, China
H.Z. Wang (1982)
Tectonic development of the continental margins on both sides of the palaeo‐Qinling marine realm, Vol.56
Cheng (1982)
Notes on the metamorphic Series and metamorphic belts of various metamorphic epochs of China and related problemsRegional Geology of China
M.P. Klimetz (1983)
Tectonics, Vol.2
Zh. Zhang, J. Liou, R. Coleman (1984)
An outline of the plate tectonics of China: Discussion and replyGeological Society of America Bulletin, 96
(1969)
Geological Map of the Qinling Mountains (1:500,000)
W. Hongzhen, Qiao Xiufu (1984)
Proterozoic stratigraphy and tectonic framework of ChinaGeological Magazine, 121
H.Q. Wu (1984)
Brief description of the high‐pressure low‐temperature metamorphic belts in China and discussions on some problems about glaucophane and barroisite
Q.S. Zhang (1979)
Poly‐phase metamorphism and formation of the Eastern Qinling Mountains
(1979)
Geotectonic Map of China (1:4,000,000)
Henno Martin, F. Eder (1983)
Intracontinental Fold Belts
C.Y. Li (1978)
Tectonic history of the Qinling and Qilian mountains, 1
H.Q. Wu (1980)
The glaucophane‐schists of the eastern Qinling and northern Qilian mountains in China, 54
(1975)
Geologic Map of Asia (1:5,000,000)
Abstract The Qinling Mountains separating the northern from the southern China plate is a key region for the study of structural evolution of eastern Asia. It is composed of the Palaeozoic fold belt in its northern part and the Variscan and Indosinian fold belts in its southern part. The evolution of the former is marked by the closure of a northward subducting oceanic basin in the early stage, followed by southward obduction of ophiolites and intracontinental thrusting during the Variscan; whereas that of the latter is represented by intracontinental, shallow crustal deformation on the basis of a large‐scale detachment structure (with a horizontal slip of at least of 100 km). Since the late Palaeozoic, however, both of the belts have been cut by a series of east‐west sinistral strike‐slip faults.
Acta Geologica Sinica (English Edition) – Wiley
Published: Sep 1, 1986
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