低丰度碳酸盐岩有效烃源岩存在的 证据及其TOC下限
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本文为国家重点基础研究规划“973”项目(编号 2011CB201102)资助的成果。


Evidences on Effective Carbonate Source Rock of Low Organic Matter Abundance and its Lower Limit of TOC
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  • 1) 中国石油大学(北京)油气资源与探测国家重点实验室,北京,102249; 2) 中国石油大学(北京)盆地与油藏研究中心,北京,102249;    
  • 1) 中国石油大学(北京)油气资源与探测国家重点实验室,北京,102249; 2) 中国石油大学(北京)盆地与油藏研究中心,北京,102249;    
  • 中国石油塔里木油田勘探开发研究院,新疆库尔勒,841000;    
  • 1) 中国石油大学(北京)油气资源与探测国家重点实验室,北京,102249; 2) 中国石油大学(北京)盆地与油藏研究中心,北京,102249;    
  • 陕西延长石油(集团)有限责任公司研究院,西安,710075    
  • 1) 中国石油大学(北京)油气资源与探测国家重点实验室,北京,102249; 2) 中国石油大学(北京)盆地与油藏研究中心,北京,102249;    
  • 1)State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Bejing, 102249; 2)Basin & Reservoir Research Center,China University of Petroleum,Bejing, 102249;    
  • 1)State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Bejing, 102249; 2)Basin & Reservoir Research Center,China University of Petroleum,Bejing, 102249;    
  • Basin & Reservoir Research Center,China University of Petroleum,Bejing, 102249;    
  • 1)State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Bejing, 102249; 2)Basin & Reservoir Research Center,China University of Petroleum,Bejing, 102249;    
  • Research Institute of Shaanxi Yanchang Petroleum(Group)Co. Ltd., Xi’an, 710075    
  • 1)State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Bejing, 102249; 2)Basin & Reservoir Research Center,China University of Petroleum,Bejing, 102249;    
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    摘要:

    中国碳酸盐岩分布面积广、热演化程度高、有机质丰度普遍较低,研究低丰度碳酸盐岩能否成为有效烃源岩对评价碳酸盐岩油气潜力和勘探前景具有重要意义。多方面研究表明,随着深度增大或热演化程度的提高,碳酸盐岩烃源岩TOC降低、生烃潜力和残留烃量均表现出先增大后减小的趋势,生烃热模拟实验结果等都表明低丰度碳酸盐岩烃源岩可以发生生排烃作用,国外勘探实践亦发现低丰度碳酸盐岩作为烃源岩的油气田,这都表明低丰度碳酸盐岩可以成为有效烃源岩。确定碳酸盐岩烃源岩TOC下限需要考虑多个因素,研究认为碳酸盐岩烃源岩的TOC下限应该比泥页岩的05%低一些。根据排烃门限,利用生烃潜力法和物质平衡数值模拟计算法确定了不同成熟阶段有效烃源岩TOC下限,结合前人研究成果和勘探实践,综合确定低成熟阶段、成熟阶段和高过成熟阶段碳酸盐岩有效烃源岩的TOC下限分别为TOC≥14%、TOC=01%~14%和TOC<01%。

    Abstract:

    The carbonate rocks are widely distributed, whose thermal evolution is generally high and organic matter abundance are lower in China. Whether or not they can be effective source rocks has great significance for the evaluation of hydrocarbon generation potential and exploration prospect of carbonate rocks. Many studies show that as the depth or thermal evolution degree increase, TOC of source rocks decreases, and hydrocarbon generation potential and residual amount increase and then decrease, besides the results of thermal simulation experiment, which indicate the source rocks of low organic matter abundance could can generate and expulse a great number of hydrocarbon. Hydrocarbon sources of some typical oil and gas fields are the carbonate rocks of low organic matter abundance in the world. A few factors could be considered to determine the lower limit of TOC of carbonate source rocks. The analysis suggests the lower limit of TOC of carbonate source rocks is less than 0.5% of mud rocks. The lower limit of TOC of the effective source rocks with different maturity was gained by the method of hydrocarbon generation potential and simulative calculation based on material balance principle according to the hydrocarbon expulsion threshold. Referring to the study results of predecessors and exploration practice, The lower limit of TOC of the effective carbonate source rocks with low maturity, maturity and high—over maturity stages respectively are TOC≥1.4%, TOC=0.1%~1.4% and TOC<0.1%.

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霍志鹏,庞雄奇,张宝收,陈践发,范柏江,李素梅.2013.低丰度碳酸盐岩有效烃源岩存在的 证据及其TOC下限[J].地质论评,59(6):1165-1176,[DOI].
.2013. Evidences on Effective Carbonate Source Rock of Low Organic Matter Abundance and its Lower Limit of TOC[J]. Geological Review,59(6):1165-1176.

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  • 收稿日期:2013-05-23
  • 最后修改日期:2013-08-16
  • 在线发布日期: 2013-11-14