关于吉普斯菌的发展,进化和主要控制因素的研究Ma541,中央奥尔多斯盆地
Jiang He1, Chuanjiang Tang1, Gang Zhao2
1School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, Sichuan, China.
ACS omega
|October 27, 2025
概括
这项研究揭示了石膏菌孔如何通过沉积物,表观遗传和埋葬过程在奥尔多斯盆地形成. 了解这些孔隙发育模式是识别高质量的碳酸盐储库的关键.
科学领域:
- 地质地质地质地质地质地
- 沉积物学的沉积物学
- 诊断发生的过程.
背景情况:
- 石膏菌孔对于碳酸盐形成中的水库发展至关重要.
- 在奥尔多斯盆地的马吉亚古 (Majiagou) 构造中含有大量碳酸盐储库.
研究的目的:
- 系统地揭示石膏菌孔的发展和演化模式.
- 确定高质量的碳酸盐储的储控制机制.
主要方法:
- 核心观察 核心观察
- 在X射线衍射 (XRD) 中.
- 碳和氧同位素分析
主要成果:
- 石膏毛孔在石膏载体多洛米特中通过叠加的二代遗传阶段发展.
- 毛孔的发展涉及合成无水沉,表观遗传流星淡水溶解和埋葬溶解扩大.
- 该研究确定了三因素的水库控制机制:石膏-多洛米特平面,有效的表观遗传溶解与弱填充,并叠加埋葬修改.
结论:
- 石膏毛孔的发育模式是由沉积物,表观遗传和埋葬代遗传过程的组合控制的.
- 鉴定的储控制机制为评估类似盆地的碳酸盐储提供了理论基础.
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