摘要
以四川盆地上二叠统为例,论述牙形石色变指标CAI在碳酸盐岩油气田勘探中的应用。由20余条实测剖面,获取了相应的CAI值,据此划分了盆地上二叠统有机质热变质的成熟期,认为广元、北川、安县一带处于成熟期;川中、川南和川东等地区处于高成熟期;成都、南充、绵阳等地区处于过成熟期。根据CAI值推算了盆地各地区的古地温,认为高值(170~400℃)区在绵阳、成都、南充、达县及旺苍等地区;低值(50~100℃)区在广元至江油以北地区;川东、川南广大地区为130~200℃。根据CAI值及古地温,推算出上二叠统顶面埋藏深度,编制了埋深等值线图,与实测结果基本吻合。综合以上推算结果,预测四川盆地上二叠统的原油、凝析油主要分布在龙门山前缘带,其余地区主要产天然气。图3表5参6(梁大新摘)
At present, based on the organic particles and microfossils, such as
sporepollen, vitrinite, kerogen, organic metamorphism in strata can be identified,
and this method is effective to mudstone, clastic rocks, but not to carbonate
rocks, conodont fossils are very common in the marine carbonate strata from
Cambrian to Triassic. It means the organic metamorphism in marine carbonate
rocks can be identified by using conodont color alteration. This method is
effective, cheap and easily. Research results of years of the s are presented in
the paper. It indicates that few common methods are useful for drawing CAI
value contour maps which are significant to the carbonate oilgas fields
exploration, for example, the conodont color alternation in carbonate strata for
Upper Permian in Sichuan basin.
出处
《石油勘探与开发》
SCIE
EI
CAS
CSCD
北大核心
1999年第2期46-48,共3页
Petroleum Exploration and Development
基金
油气藏地质及开发工程国家重点实验室开放基金
关键词
碳酸盐岩
油气田勘探
牙形石
色变
Sichuan basin, Upper Permian
series, Carbonate rock, Conodont color alteration index, Organic matter maturity,
Paleotemperature, Burial depth, Oil and gas distribution, Prediction