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中国海相碳酸盐岩评价中有关有机质丰度下限的几点讨论
引用本文:刘华,彭平安,刘大永,林玉祥.中国海相碳酸盐岩评价中有关有机质丰度下限的几点讨论[J].地质通报,2006(Z2).
作者姓名:刘华  彭平安  刘大永  林玉祥
作者单位:中国科学院广州地球化学研究所,中国科学院广州地球化学研究所,中国科学院广州地球化学研究所,中石化胜利油田有限公司地质科学研究院 广东广州510640中石化胜利油田有限公司地质科学研究院,山东东营257015,广东广州510640,广东广州510640,山东东营257015
基金项目:国家油气专项之《华北前第三系油气资源战略调查及评价》课题(编号:XQ-2004-03)资助。
摘    要:综述了中国海相碳酸盐岩有机质下限研究的若干进展,认为针对不同需求,应提出碳酸盐岩烃源岩最低下限、有效烃源岩下限、战略选区下限3个不同的下限标准。高成熟碳酸盐岩原始有机质丰度恢复一直存在争议,根据生烃动力学,结合热史,可实现原始有机质总量的恢复。碳酸盐岩中泥质与有机质丰度、排烃能力是否相关仍存在争论,认为碳酸盐岩中泥质的作用仍有待进一步研究。

关 键 词:海相碳酸盐岩  烃源岩评价  下限  有机质丰度恢复

Threshold of the organic matter abundance in marine carbonate source rocks in China
LIU Hua,PENG Ping-an,LIU Da-yong,LIN Yu-xiang . Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou ,Guangdong,China, . Research Institute of Geological Sciences,Shengli Oilfield Corporation Ltd.,SINOPEC,Dongying ,Shandong,China.Threshold of the organic matter abundance in marine carbonate source rocks in China[J].Geologcal Bulletin OF China,2006(Z2).
Authors:LIU Hua    PENG Ping-an  LIU Da-yong  LIN Yu-xiang Guangzhou Institute of Geochemistry  Chinese Academy of Sciences  Guangzhou  Guangdong  China  Research Institute of Geological Sciences  Shengli Oilfield Corporation Ltd  SINOPEC  Dongying  Shandong  China
Institution:LIU Hua1,2,PENG Ping-an1,LIU Da-yong1,LIN Yu-xiang2 1. Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China, 2. Research Institute of Geological Sciences,Shengli Oilfield Corporation Ltd.,SINOPEC,Dongying 257015,Shandong,China
Abstract:This paper reviews some advances in the study of the organic matter thresholds of marine carbonate rocks in China. The authors think that for different demands there should be three different thresholds, i.e. the lowest threshold for marine carbonate source rocks, threshold for effective source rocks and threshold for strategic area selection. Reconstruction of the original organic matter abundance in high-mature marine carbonate rocks has long been in dispute. Hydrocarbon-generating kinetics, combined with the thermal history, may provide a good approach to this purpose. Whether the clay content plays an important role in the enrichment of organic matter in carbonate source rocks and expelling capacity of hydrocarbon is still in dispute. The authors think that the role of the clay content in carbonate rocks remains to be further studied.
Keywords:marine carbonate rocks  evaluation of source rocks  threshold  reconstruction of the organic matter abundance
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