在古世织河流三角洲的演化和石油系统的构造气候控制,在Lenghu构造带,北Qaidam盆地
Lei Gong1,2,3, Wenhai Gai4, Xianzhi Gao5,6
1School of Highway and Construction Engineering, Yunnan Communications Vocational and Technical College, Kunming, 650500, China. leigong0607@126.com.
Scientific reports
|August 25, 2025
概括
卡伊达姆盆地的古世河流三角洲沉积物显示,从潮湿的淡水环境转变为半干旱的水环境. 这种转变对区域石油系统产生了重大影响,因为它改变了水库质量和源岩潜力.
科学领域:
- 沉积地质学
- 地质化学
- 地质学
背景情况:
- 在Lenghu构造带的古世河沉积物是了解Qaidam盆地的石油系统的关键.
- 沉积过程中的环境条件影响了水库结构和源岩潜力.
研究的目的:
- 研究古气候,古盐度,古状况,起源和古沉积物进化.
- 了解环境转型及其对石油系统的影响.
主要方法:
- 石化分析 (薄截面,重矿物质)
- 地化学分析 (微量元素和稀土元素).
- 地质物理方法 (井口记录,2D地震解释).
主要成果:
- 从潮湿的,淡水的,有氧的到半干旱的,的,有氧的条件的转变.
- 确定了萨西山作为主要的沉积物来源,提供中间岩石.
- 记录了从织的河流转向带有薄床沙体的湖泊三角洲.
结论:
- 构造气候合,干燥增强的蒸发性密封,以及火热来源控制水库架构和石油系统的演变.
- 这项研究提供了类似湖泊环境的见解.
- 了解这些因素对于区域石油勘探至关重要.
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