三阶段的构造进化控制了在西爪逆弧盆地中碳化合物的差异分布
Zengyuan Zhou1,2, Wenxu Peng3, Hefeng Sun3
1State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China.
西爪盆地的碳化合物分布主要由沉降期间的源岩分布控制. 构造学发展和岩石形成影响了该石油省的碳化合物产生和积累.
科学领域:
- 地质地质地质地质地质地
- 石油地质科学 石油地质科学
- 构造学 构造学 构造学 构造学
背景情况:
- 西爪盆地是东南亚的一个重要的石油省份.
- 最近的发现表明,新的碳化合物储量正在增加.
- 了解资源分布和构造进化对于勘探至关重要.
研究的目的:
- 系统地探索西爪盆地的碳化合物资源分布和构造演变.
- 分析碳化合物分布的主要控制因素.
- 在不同区块中划分石油和天然气的形成和分布.
主要方法:
- 对构造进化特征的分析.
- 研究源岩的分布及其对沉积层的影响.
- 评估热流和 magma 对碳化合物产生的影响.
- 石油和天然气类型的划分及其分布.
主要成果:
- 碳化合物的分布不均,主要由沉降期间的源岩分布控制.
- 一个小小的东西.
- 三个阶段的三个阶段.
- 构造发展过程影响源岩和沉积面的分布.
- 地的削弱和磁性增强热流,加速碳化合物生成.
结论:
- 沉降期间的源岩分布是碳化合物模式的主要控制因素.
- 构造学发展和岩活动是碳化合物生成的关键因素.
- 潜在的勘探区域包括中南部浅深水域和未经探索的陆地区域.
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