石油学报 ›› 1982, Vol. 3 ›› Issue (1): 1-9.DOI: 10.7623/syxb198201001

• 地质勘探 •    下一篇

碳酸盐岩有机质演化特征与油气评价

傅家谟, 刘德汉   

  1. 中国科学院地球化学研究所
  • 收稿日期:1980-08-18 出版日期:1982-01-25 发布日期:2013-07-08

SOME CHARACTERISTICS OF THE EVOLUTION OF ORGANIC MATTER IN CARBONATE FORMATIONS

Fu Jiamo, Liu Dehan   

  1. Institute of Geochemistry, Academia Sinica
  • Received:1980-08-18 Online:1982-01-25 Published:2013-07-08

摘要: 在中国东部广泛发育一套巨厚碳酸盐岩地层(震旦系至三迭系)。本文扼要探讨了碳酸盐岩有机质早期演化特征之一——有机质的大量成岩丢失及其与碳酸盐岩分布地区油气远景评价之关系。作者还叙述了晚期演化阶段碳酸盐岩有机质,如气体烃、可溶有机质与干洛根的演化特征。根据川南地区油气的垂直分布情况,提出了碳酸盐岩地层中工业油、气的保存下限。

Abstract: Widespread in East China is a suite of well-developed and very thick carbonate formations(from Sinian to Triassic).In the present paper a brief discussion has been gieven to one of the characteristic features of the early evolution of organic matter in carbonate rocks——the great diagenetic loss of organic matter and its bearing on the evalution of oil and gas prospects in carbonate rock-distributed areas.The authors have also described the characteristic features of the evolution of organic matter,such as gaseous hydrocarbons,souble organic matter and kerogen in the carbonate rocks which have evidently reached the late stage of organic evolution,as well as the highest temperature range they once underwent during their evolution history.In terms of the vertical distribution patterns of oil and gas.in the region of South Sichuan,the lowest limit has been prelimarily established for the commercial preservation of oil and gas in carbonate formations.