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Wang Guochen (1985)
Characteristics of faults and oil and gas in East China Sea BasinSeismic Geology for Oil, 1
Guo Lingzhi (1983)
On the formation and evolution of the Mesozoic‐Cenozoic active continental margin and island‐arc tectonics of the western Pacific OceanActa Geologica Sinica, 57
T. Harding (1984)
Graben Hydrocarbon Occurrences and Structural StyleAAPG Bulletin, 68
The East China Sea Basin is a major Cenozoic basin, with a sedimentary fill greater than 10,000 metres in thickness. The evolution of the basin is divisible into four stages‐down‐faulting, fault‐sagging, down‐warping and draping. Tectonic movements were characterized by multiple episodes of spatial differentiation, and tectonic units are divisible into longitudinal zones and latitudinal blocks. Various types of trap structure are present, including Tertiary sandstone traps, basement traps, and reef traps.
Journal of Petroleum Geology – Wiley
Published: Jan 1, 1990
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