The Tectonic Inversion Prediction in Fold-and-Thrust Belts by Using Numerical Modeling

IF 1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geotectonics Pub Date : 2024-08-29 DOI:10.1134/s001685212470033x
S. F. A. Zaidi, N. Ahsan
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Abstract

This research investigates tectonic inversion in rifted continental margins, specifically focusing on the interaction between foreland sediment deposits and fold-and-thrust belts during orogeny. Using numerical modeling with ANSYS-2023 R1 software and a Maxwell-type viscoelastic rheology, the study explores positive inversion in petroleum basins, revealing insights into the evolution of inverted basins. The research emphasizes the role of pre-existing extensional fault systems in controlling thrust faults, delving into the reactivation of faults and uplift of the hanging wall during tectonic compression. The study highlights diverse structural patterns associated with tectonic inversion in sub-thrust regions of fold-and-thrust belts, including anticlines, back-thrusts, fault propagation folds, pop-up, and an inversion-related fracture pattern. Results demonstrate the critical influence of rheological properties in fault reactivation and deformational styles during tectonic inversion. Comparisons with natural case studies, like the Helvetic nappes in Switzerland, validate the predictive capability of numerical models for tectonic inversion structures in different geological settings, including the Kohat-Potwar Fold and Thrust Belt in Pakistan. We find important of understanding interplay between geological structures and rheological properties for accuracy of predicting evolution of inverted basins. The deeply study of tectonic inversion are extending to optimizing exploration efforts and interpreting structural complexities in petroleum exploration, providing valuable insights for reservoir prediction and fold-and-thrust belt structural evolution.

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利用数值建模预测褶皱推覆带的构造反演
摘要 本研究调查了断裂大陆边缘的构造反演,特别侧重于造山运动期间前陆沉积与褶皱推覆带之间的相互作用。该研究利用 ANSYS-2023 R1 软件和 Maxwell 型粘弹性流变学进行数值建模,探讨了石油盆地的正反转,揭示了反转盆地演化的深刻内涵。研究强调了原已存在的伸展断层系统在控制推力断层方面的作用,深入探讨了构造压缩过程中断层的重新激活和悬壁的隆起。研究强调了与褶皱推覆带次推覆区构造反演相关的各种构造模式,包括反褶、反推、断层扩展褶皱、弹出以及与反演相关的断裂模式。研究结果表明,在构造反演过程中,流变特性对断层再活化和变形方式有着至关重要的影响。通过与瑞士赫尔维蒂褶皱带等自然案例研究的比较,验证了数值模型对不同地质环境下构造反转结构的预测能力,包括巴基斯坦的科哈特-波特瓦褶皱与推覆带。我们发现,了解地质结构和流变特性之间的相互作用对于准确预测倒置盆地的演变非常重要。对构造反演的深入研究将扩展到优化勘探工作和解释石油勘探中的构造复杂性,为储层预测和褶皱推覆带构造演化提供宝贵的见解。
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来源期刊
Geotectonics
Geotectonics 地学-地球化学与地球物理
CiteScore
1.90
自引率
9.10%
发文量
28
审稿时长
3 months
期刊介绍: Geotectonics publishes articles on general and regional tectonics, structural geology, geodynamics, and experimental tectonics and considers the relation of tectonics to the deep structure of the earth, magmatism, metamorphism, and mineral resources.
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