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《ACTA SEDIMENTOLOGICA SINICA》 2000-03
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The Division of High-resolution Sequences and the Transgressive Coal Formation in the Epicontinental Basin of the Western Shandong Province

LI Zeng xue WEI Jiu chuan HAN Mei lian (Shandong Uniuersity of Science and Technology,Tai'an Shandong 271019)  
The high-frequency sea level changes in the North China epicontinental basin from the Late Carboniferous to Early Permian are the main factors controlling the basin-filling and coal accumulation. The coal-bearing succession, therefore, has distinct cycles. The sea level changes in the North China epicontinental basin were composite sea level changes. The long-term sea level changes are superposed by shorter-term cycles, the mid-term and short-term sea level changes. There were short-term retrogressive events in the process of long term transgressive period, and multiple short periodic transgressive events superposed on the long-term transgressive period. Study shows that the base-level cycles in the North China epicontinental basin may be substitute by the relative sea level cycles, because the high-frequency sea level changes in the basin are the integrative results of the sea level changes, the tectonic subsidence, the climate changes and the sediment supply. The later three factors, the tectonics, the climate and the sediment supply were relatively stable. The sea level changes, thus, become the dominant factor. Using the thought and methodology of high-resolution sequence stratigraphy, the authors investigate the characteristics of the high-resolution sequence stratigraphy of the coal measures in the Western Shandong, identify and divide the mid-long term and mid-short term base-level cycles. Three long-term base-level changes lead to the formation of three third order sequences. The mid-term base-level cycles are approximately corresponded to the systems tracts. Large-scale marine flooding events were caused by the mid-term base-level rise. Because of the hysteresis of the deposition, the thick-bedded limestones were deposited in the period of maximum base-level rises, which occurred three times in the history of the epicontinental basin, representing the depositions of three times of maximum base-level rises. The outstanding feature of the paralic succession is the alternative occurrences of the marine and terrestrial depositions, forming multiple cycles. That the marine layers directly superposed on the coalbeds is another feature of the deposition in the epicontinental basin. Eighteen short-term base-level cycles may be recognized in the epicontinental succession of the Western Shandong. Most of cycles are asymmetric, seperated by episodic transgressive event surfaces, peatification event surfaces and large scope of scouring surfaces. The short-term base-level cycles are of high frequency. The identification and correlation of short-term base-level cycles help to the division of high-resolution sequence. The study of the epicontinental paralic base-level cycles in the Western Shandong indicates that the eighteen short-term base-level cycles are corresponded to eighteen fifth-order sequences (corresponding to the parasequences). The episodic transgressive events have great effect on the coal accumulation in the epicontinental basin; coal formation in the transgressive process is the outstanding feature of the coal formation in the Western Shandong coalfields. The transgressive coalbeds in the long-term base-level cycles develop in the transgressive systems tracts, while the transgressive coalbeds in the short-term base-level cycles occur in the high stand systems tracts.
【Fund】: 国家自然科学基金项目!(批准号 :49872 0 57)资助
【CateGory Index】: P539.2
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