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Article Navigation >  Acta Sedimentologica Sinica  > 2005  >  23(1): 29-33

YAN ZhenYANG, Chang-chunLI, Ji-liang, WANG Zhen-li, XIAO Wen-liao, XU Xing-wang, DUAN Qiu-liang. Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 29-33.
Citation: YAN ZhenYANG, Chang-chunLI, Ji-liang, WANG Zhen-li, XIAO Wen-liao, XU Xing-wang, DUAN Qiu-liang. Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 29-33.
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Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province

  • Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029

  • Received Date: 2004-03-09
  • Rev Recd Date: 2004-06-02
  • Publish Date: 2005-03-10
  • The Mantou Format ion in the North China platform, which overlain the Archaean Taishan Group, mainly consists of terrigenous clastic rocks and carbonate interca lations. In the Zhonggong village of the Jinan city, olistotrome with thickness of about 4m occurred in 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 bedding within the blocks demonstrate that there should ex ist an old slope in the North China platform and tectonic uplifting had took place in the Cambrain. They were main factors to induce olistotrome. Identifying and studying the olistostrome with in the Mantou Formation is benefit to study the Paleozoic paleogeography and sedimentary env ironments of the North China platform and the evolution of the buried hills, which can provide some good evidences for the study on the Paleozoic sedimentary basin contained with abundant oil and gas and buried hills, and for prospecting source of oil and gas.
  • [1] 1 山东省地质矿产局. 山东省区域地质志[M].北京:地质出版社,1982.1-594.

    2 FloresG. Discussion: Proceedings of the 4th World Petroleum Conference[C].1955.121-122.

    3 MorgensternSNR. Submarine slumping and initiation of turbidity currents[A].Urbana:University of Illinois Press,1967.189-220.

    4 RyanWF,Von Rad U. Passive continental margin Preliminary Report Leg 47[N].Geo times,1977.

    5 NaylorMA. Debris flow olistostromes and slumping on a distal passive continental margin: the Palombini limestone0shale sequence of the northern Apennines[J]. Sedimentology, 1981. 837-852.

    6 CookHE. Ancient continental slope sequences and their value in understanding modern slope development [M].Doyle L J Pikey O H eds Geology of Continental Slope Spec Publ Soc Econ Paleon Miner 27,1979.
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Publishing history
  • Received:  2004-03-09
  • Revised:  2004-06-02
  • Published:  2005-03-10

Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province

  • Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029
  • Received Date: 2004-03-09
  • Rev Recd Date: 2004-06-02
  • Publish Date: 2005-03-10

Abstract: The Mantou Format ion in the North China platform, which overlain the Archaean Taishan Group, mainly consists of terrigenous clastic rocks and carbonate interca lations. In the Zhonggong village of the Jinan city, olistotrome with thickness of about 4m occurred in 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 bedding within the blocks demonstrate that there should ex ist an old slope in the North China platform and tectonic uplifting had took place in the Cambrain. They were main factors to induce olistotrome. Identifying and studying the olistostrome with in the Mantou Formation is benefit to study the Paleozoic paleogeography and sedimentary env ironments of the North China platform and the evolution of the buried hills, which can provide some good evidences for the study on the Paleozoic sedimentary basin contained with abundant oil and gas and buried hills, and for prospecting source of oil and gas.

YAN ZhenYANG, Chang-chunLI, Ji-liang, WANG Zhen-li, XIAO Wen-liao, XU Xing-wang, DUAN Qiu-liang. Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 29-33.
Citation: YAN ZhenYANG, Chang-chunLI, Ji-liang, WANG Zhen-li, XIAO Wen-liao, XU Xing-wang, DUAN Qiu-liang. Geological Features and Significance ofOlistostromes from Lower Part of the Mantou Formation in the LuxiAreas, Shandong Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 29-33.
shu

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