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《Acta Sedimentologica Sinica》 2005-01
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Geological Features and Significance of Olistostromes from Lower Part of the Mantou Formation in the Luxi Areas, Shandong Province

YAN ZhenYANG Chang-chunLI Ji-liang WANG Zhen-liXIAO Wen-liaoXU Xing-wangDUAN Qiu-liang (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029)  
TheMantou Formation in the North China platform, which overlain the Archaean Taishan Group, mainly consists of terrigenous clastic rocks and carbonate intercalations. In the Zhonggong village of the Jinan city, olistotrome with thickness of about 4m occurredin the lower part of the Mantou Formation. Carbonate and fine clastic rocks is its block, and siltstone is its matrix. Deformation styles of the blocks and cross beddingwithin the blocks demonstrate that there should exist an old slope in the North China platform and tectonic uplifting had took place in the Cambrain. They were main factors toinduce olistotrome. Identifying and studying the olistostrome within the Mantou Formation is benefit to study the Paleozoicpaleogeography and sedimentary environments of the North China platform and the evolution of the buriedhills, which can provide some good evidences for the study on the Paleozoicsedimentary basin contained with abundant oil and gas and buriedhills, and for prospecting source of oil and gas.
【Fund】: 中国科学院知识创新项目“环渤海(湾)地区前新生代海相典型含油气区剖析(KZCX1-SW-18)”资助。
【CateGory Index】: P512.2
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1 Shou Hao1 , Liu Hong1, and Gao Jianhu121. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.. 2. Northwest Institute, Research Institute of petroleum Exploration and Development, PetroChina, Lanzhou 730000, China.;AVO inversion based on common shot migration[J];应用地球物理(英文版);2006-02
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