LI Yan-ping, LIN Zhen-hong, CHEN Shu-min, SONG Yong-zhong, ZHANG Er-hua, SHEN Jia-gang. CLIMATIC SEQUENCE CHARACTERS OF CLOSED DEPRESSION LACUSTRINE BASIN[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 91-96.
Citation: LI Yan-ping, LIN Zhen-hong, CHEN Shu-min, SONG Yong-zhong, ZHANG Er-hua, SHEN Jia-gang. CLIMATIC SEQUENCE CHARACTERS OF CLOSED DEPRESSION LACUSTRINE BASIN[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 91-96.
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CLIMATIC SEQUENCE CHARACTERS OF CLOSED DEPRESSION LACUSTRINE BASIN

  • 1 College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;

  • 2 Qinghuangdao Branch of Daqing Petroleum College, Qinhuangdao 066004, China;

  • 3 Exploration and Development Research Institute of Daqing Oilfield Company Ltd. Daqing 163712, China

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  • Received Date: July 14, 2007
  • Revised Date: October 14, 2007
    Graphical Abstract
    • Abstract
  • Closed depression lacustrine basin is mainly characterized by climatic sequence.In idealistic conditions, three-grade climatic periodic changes basically conform to sine curve. Type Ⅰclimatic sequence of an integrated closed depression lacustrine basin is composed of four parasequences:LPWST,TST,HST and FRWST. Similarly, type Ⅱclimatic sequence of an integrated closed depression lacustrine basin is composed of 3 parasequences:TST,HST and FRMST. These tracts have relevant locations in curves of climatic periodic changes and sequence boundary is at the lowest point of base-level changes.
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    • References (10)
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