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《Geological Review》 1990-05
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DISCOVERY OF SLIDING STRUCTURES ON THE PLANE OF UNCONFORMITY BETWEEN THE LOWER PALAEOZOIC AND THE TAISHAN GROUP IN THE VICINITY OF TAISHAN MOUNTAINS

Lu Pengju, Zhang Mingli and Zhu Xingshan(Dept. of Geol., Shandong Institute of Mining & Technology, Tai'an, Shandong)  
In recent years, the authors have discovered a lot of sliding structures on the plane of unconformity between the Lower Palaeozoic and the Archean Taishan Group in the vicinity of Taishan Mountains. The plane of unconformity is a slide surface a ong which there are a lot of slide breccia and elastic dikes and on which there are a lot of striations and polished surfaces. The hanging wall of the Palaeozoic is a sliding system with complicated structures. Moderately thick dolomitic limestone bearing chert bands and thin bedded dolomitic marl at the base of the Cambrian Mantou Formation were folded and some of them disappeared due to sliding. The foot-wall is an autochthonous system having simple structures. There is only some cataclasite in it. After analysing the features of sliding structures, the authors think that they are gravitation sliding structures caused by tilting of fault blocks, and the hanging side moved to the north after the Yanshanian movement. This discovery explains from a tectonic view of point why some beds at the bottom of the standard section of the Cambrian at Zhangxia, Changqing, are absent, which is of major significance for carrying out the study of sliding structures in western Shanddong and gaining a further knowledge of the tectonics therein.
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