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巴西桑托斯盆地盐下层序油气地质特征与有利区预测

邬长武

石油实验地质Issue(1):53-56,63,5.
石油实验地质Issue(1):53-56,63,5.DOI:10.11781/sysydz201501053

巴西桑托斯盆地盐下层序油气地质特征与有利区预测

Petroleum geology characteristics and exploration targets of pre-salt formations in Santos Basin, Brazil

邬长武1

作者信息

  • 1. 中国石化 石油勘探开发研究院,北京 100083
  • 折叠

摘要

Abstract

The Santos Basin in Brazil has experienced three tectonic evolution stages ( rifting, transitional and passive continental) with three sequences deposited ( pre⁃salt, salt and post⁃salt) . Source rocks in the pre⁃salt formations in the lower rift were the most effective source rocks in the basin. Microbial limestones in the upper rift and depression, and coquina limestones in upper rift served as the main reservoirs for the pre⁃salt source rocks. The salt formations had strong capping capacity thanks to great thickness and continuous distribution in the deep water area. The basement horst belt helped the formation of various structural traps. All these advantageous geo⁃logic conditions provided a good basis for the generation of giant oil and gas pools in the pre⁃salt formations in the basin. The basement horst belt in the deep water area in the north of the basin was a favorable location for the pre⁃salt hydrocarbon accumulation, where the source rocks were moderately mature, and the thick, continuously distributed salt formations provided a good preservation environment. In the shallow water area formed by a base⁃ment horst, carbonate reservoirs were well⁃developed, and traps such as horsts, tilted fault blocks and drape an⁃ticlines were very common. Hydrocarbons generated in the surrounding grabens migrated to and accumulated in the horsts. The other pre⁃salt formations had poor accumulation conditions.

关键词

油气地质特征/成藏模式/油气分布/盐下/桑托斯盆地

Key words

petroleum geologic characteristics/hydrocarbon accumulation pattern/hydrocarbon distribution/pre-salt/Santos Basin

分类

能源科技

引用本文复制引用

邬长武..巴西桑托斯盆地盐下层序油气地质特征与有利区预测[J].石油实验地质,2015,(1):53-56,63,5.

基金项目

中国石化科技部项目“巴西重点盆地油气资源潜力及选区评价”( P11063)资助。 ()

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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