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Daiyong Daiyong, Wenxia Wenxia (1990)
Technology of the anisotropy of the reflectivity of vitrinite and its application to the study of structureCoal Geology of China, 2
Fenggen Fenggen, Hongcai Hongcai (1986)
The Tertiary nappe structure in Nujiang, Lancangjiang and Jinshajiang RegionBulletin of Nanjing Institute of Geology and Mineral Resources, CAGS. Supplement No, 1
C. Onasch (1986)
Ability of the Fry method to characterize pressure-solution deformationTectonophysics, 122
F. Odonne (1990)
The control of deformation intensity around a fault: natural and experimental examplesJournal of Structural Geology, 12
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Jointing and fracture interactions in middle eocene chalks near beer sheva, IsraelTectonophysics, 136
C. Onasch (1990)
Microfractures and their role in deformation of a quartz arenite from the central Appalachian forelandJournal of Structural Geology, 12
Abstract The arcuate nappe structure on the north edge of the Wuliang Mountains in western Yunnan Province is a complex nappe structural system with multiple superimposed structures. The autochthonous system is a WNW—trending arcuate fold belt consisting of the Jurassic and Cretaceous and the allochthonous system is mainly composed of Upper Triassic rocks. Generally, the nappe structure moved from south to north, with the hanging wall thrusting in a WNW direction for a distance of over 10 km. The deep nappe structural system was formed at depths of about 5–10 km in an environment not exceeding the greenschist facies. It occurred in the Oligocene (about 40‐20 Ma).
Acta Geologica Sinica (English Edition) – Wiley
Published: Jun 1, 1996
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