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《ACTA SEDIMENTOLOGICA SINICA》 1998-04
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History of Regional Tectonic Subsidence and Sea Level Changes in Geological History

Zhao Yuguang (Chengdu Institute of Geology and Mineral Resources,Chengdu Sichuan 610082)  
The history of regional tectonic subsidence and sea level changes are two major factors of four factors in sequence stratigraphy.The dynamic model of tectonic subsidence curves from the Devonian to the Triassic in the study area has been reconstructed by the approach of back stripping.The evolution succession of the basin ,which is from the passive continental margin,mature passive continental margin ,peripheral foreland basin to post orogeny foreland basin ,is identified.At the same time ,the curves of sea level changes in the Permian and Triassic have been inversed by the information of sedimentary systems tract, seismic section and isotope of carbon and oxygen.The sea level changes in the study area are in synchronism with the global sea level changes.The period of sea level rising in the study area lasts to Changxingian Age of Late Permian and the time of sea level falling is Dalong Age of Late Permian.The sea level changes of Late Triassic in the study area are rising and the global sea level chenges is mainly in falling stage.It is relative to the orogenic overthrusting.
【CateGory Index】: P736.22,P534.46
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