ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青藏高原油气勘探战略选区和战术突破目标的建议
  
关键词:Tibet  hypothesis of one basin between two oldlands  Coqen Block  Baoji oil-bearing assemblage  oil and gas exploration
基金项目:国家自然科学基金项目(编号: 41472030);科技基础性工作专项(编号: 2015FY310100);中国地质调查局基础性公益性矿产地质调查项目(编号: DD20160120-02; DD20160120-04; DD20160126);中国地质科学院基本科研业务费项目(编号: J1607)
作者单位E-mail
纪占胜 中国地质科学院 jizhansheng@vip.sina.com 
武桂春 中国地质科学院地质研究所, 国土资源部地层与古生物重点实验室  
姚建新 中国地质科学院地质研究所, 国土资源部地层与古生物重点实验室  
孙倩 中国地质大学(北京)
中国地质科学院 
 
石秋圆 中国地质科学院
中国地质大学(北京) 
 
何继富 中国地质大学(北京)
中国地质科学院 
 
李浩 中国地质科学院
中国地质大学(北京) 
 
刘振宇 吉林省地质调查院  
郭安臣 吉林省地质调查院  
侯召硕 吉林省地质调查院  
李东泽 吉林省地质调查院  
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摘要:
Suggestions on the Strategic Selection of Petroleum Target Areas and the Tactic Breakthrough of the Oil and Gas Exploration in the Tibetan Plateau
      The geological hypothesis of three oldlands separated by two troughs has long been the guiding theory for the oil and gas exploration of the Tibetan Plateau. The core pillar of the hypothesis is that Gangdise region was an oldland (the Gangdise Oldland) during Late Permian to Jurassic. The oldland was interpreted by the argument that the strata of the upper Permian and the Middle–Upper Jurassic are terrestrial facies and the strata of the Triassic and lower Jurassic failed to deposit. However, many marine strata previously thought to be not deposited have been identified by biostratigraphic investigations, which proves that the Gangdise Oldland does not exist actually. The absence of the Gangdise Oldland means that the above hypothesis does not represent the actural aspects of the geological pattern of the Tibetan Plateau. A new hypothesis of one basin between two oldlands is proposed in this paper. This hypothesis is mainly characterized by the argument that marine sediments deposited on the so-called Gandise Oldland. Guge Basin seems to have been the unique marine basin from Paleozoic to Mesozoic in the Tibetan Plateau. The Coqen Block in the Guge Basin had favorable geological conditions to form a large hydrocarbon province because of the existence of the Guge oil-bearing assemblage and the Baoji oil-bearing assemblage. These two assemblages comprise sediments of carbonate platform facies with hydrocarbon shows in the ourcrops and are well preserved by the Cretaceous strata which constitute the main outcrops. The Cretaceous and the strata below were compressed to form compound anticlinal structure by the NS-trending tectonic movement of Late Yanshanian–Himalayan period. The core of the anticline is the favorable structural part of the oil and gas exploration. The anticline structure was tilted to form nose structure by the EW-trending fault later. The structural high point of the nose structure is the target position for oil and gas exploration. The strategic petroleum target area selection in the Tibetan Plateau is suggested to be transferred from the Qiangtang Block to the Coqen Block, and geophysical exploration and drilling verification should be conducted on the identified nose structure in the Baoji area.
JI Zhan-sheng,WU Gui-chun,YAO Jian-xin,SUN Qian,SHI Qiu-yuan,HE Ji-fu,LI Hao,LIU Zhen-yu,GUO An-chen,HOU Zhao-shuo,LI Dong-ze.2018.Suggestions on the Strategic Selection of Petroleum Target Areas and the Tactic Breakthrough of the Oil and Gas Exploration in the Tibetan Plateau[J].Acta Geoscientica Sinica,39(4):387-400.
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