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Zhongyuan Zhongyuan (1984)
Structural pattern and evolution of Bohaiwan basin, ChinaActa Petrolei Sinica, 5
Hongzhen Hongzhen, Yang Yang, Sitian Sitian (1983)
Mesozoic and Cenozoic basin formation in East China and adjacent regions and development of the continental marginActa Geologica Sinica, Vol.57
M. Bott (1976)
Formation of Sedimentary Basins of Graben Type by Extension of the Continental CrustTectonophysics, 36
Lianshen Lianshen (1982)
Tectonic evolution of the lithosphere plates and some features of the sedimentary distribution in Cenozoic Era in South China SeaMarine Geological Research, 2
Zhou Zhou, Yin Yin (1985)
A geological review of the East China Sea and its petroleum potentialOil and Gas Geology, 6
K. Otsuki (1985)
Plate Tectonics of Eastern Eurasia in the Light of Fault SystemsThe science reports of the Tohoku University, 55
Xun Xun (1982)
Recognition of the Yanshanian movement in the eastern part of ChinaGeological Review, 28
Xun Xun (1983)
The sedimentary formation and tectonic development of the Meso‐Cenozoic in eastern ChinaRegional Geology of China
Zhanxun Zhanxun, Daoyi Daoyi, Qingyu Qingyu (1965)
Glossary of the Terms of Crustal Movements of ChinaGeological Review, 23
Abstract Since Jurassic, intense and repeated tectonic movements have taken place in eastern China, of which the Yanshanian movement is the most important. Thereby the development of the basins between the Jurassic and Eogene in the studied areas may by divided into two different stages, i.e. the Yanshanian subcycle (J‐K11) and the North China subcycle (K21‐E). The basement and tectonic stress field of the basins played an obvious role in controlling the sedimentary‐tectonic development of the basins, and down‐faulted basins might form under different stress states. Besides, the shearing stress also played an important part while the basins were forming in the noted areas.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1988
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