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《Chinese Journal of Geology》 1991-03
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TECTONIC-SEDIMENTATION RESPONSES OF THE ANYUAN COAL SERIES, NORTH JIANGXI

Wang Qingchen, Peng Haipo and Sun Shu(Insricute of Geology, Academia Sinica 100029)  
The famous Anyuan Coal Series was deposited during the so-called Indosinian Movement, when the South China Block collided with and overthrust onto the Yangtze Block in early Mesozoic. The response of the Anyuan Coal Series in the process of its sedimentation to the Mesozoic collision tectonics is discussed in the present paper.The northwestword multiple nappe-thrusting in provenance, which resulted from conti-nen-continent collision, caused the variation in sedimentary thickness and rate. In front of the nappe, sedimentary rate was slower and hickness smaller, with some unconformities developed. On the contrary, in distal area, sedimentary rate was faster and thickness larger, without any unconformity. At the same time, the northwestward thrust of nappes resulted in migration of the sedimentary facies zone in the same direction. By thrusting, the nappes lifted and underwent erosion. Their decollement history is reflected in the vertical variation in conglomerate composition in the Anyuan Coal Series.The research is a part of the China-Swiss cooperative program, which is financially supported by both the Chinese National Natural Science Foundation and the Swiss Federal Institute of Technology.
【Fund】: 中国国家自然科学基金会;; 瑞士联邦理工学院
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