在中国西部奥尔多斯盆地的奥尔多维纪层的古环境重建的基本采伐证据
Zhenyu Zhao1, Xia Zhao1, Wei Song1
1Research Institute of Petroleum Exploration and Development, PetroChina, Beijing, 100083, China.
Scientific reports
|August 28, 2025
概括
奥尔多斯盆地的奥尔多维纪层具有重要的页岩气潜力. 古环境分析揭示了有机物丰富的有利条件,指导了未来的探索策略.
科学领域:
- 地质化学
- 沉积物学
- 古代海洋学
背景情况:
- 西部奥尔多斯盆地的奥尔多维纪碳酸盐连续性是非常规碳化合物勘探的关键区域.
- 乌拉利克岩层特别以其页岩气的潜力而闻名.
研究的目的:
- 为了重建西部奥尔多斯盆地的古环境演变.
- 找出控制乌拉式形成中的有机物质丰富的因素.
- 评估奥尔多维纪层的碳化合物潜力.
主要方法:
- 从MJ1井的高分辨率元素记录数据.
- 分析主要和微量元素的分布.
- 应用地化学代理 (Al/Ti,Cu/Al,U/Th,Sr/Cu,Rb/K) 来推断古环境条件
主要成果:
- 地化学特征表明石质,生产力,氧化还原条件,古气候,盐度和水深的变化.
- 乌拉式形成表现出高的古物生产力,对亚氧氧化条件有毒,半干旱的气候和温和的水深.
- 一个从Sandaokan到Wulalike形成的跨越序列被确定,与相关的面部和地化学转移.
结论:
- 在Wulalike形成的沉积过程中存在有机物积累的有利条件.
- 这项研究提供了关于奥尔多维纪层的沉积演变和碳化合物潜力的见解.
- 这些发现对奥尔多斯盆地的页岩气勘探具有重要意义.
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