地层间断的地球物理记录混乱行为:印度上阿萨姆大陆架案例研究

IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Bappa Mukherjee , V. Srivardhan , Kalachand Sain , Aditi Gupta
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引用次数: 0

摘要

我们提出了一种新颖的分形分析辅助地层特征描述方法,以了解油气储层的原位地下地质情况。通过采用相关维度和多分形去趋势波动分析,我们量化了地球物理测井的自相似性和长程依赖性,反映了上阿萨姆盆地博格帕拉油田地层固有的独特沉积过程。与不同地层单元相关的测井曲线的分形属性被用来建立基于分形的地层特征。根据从 1.98 到 1.13 的相关维度,所研究地层的层次结构如下:Girujan > Tipam > Barail > Kopili > Prang > Narpuh > Lakadong-Therria.此外,频谱宽度值从 0.70 到 2.04 不等,反映了每个地层的空间相关性、地质复杂性和内在异质性:Kopili > Prang > Narpuh > Barail > Girujan > Tipam > Lakadong-Therria。这种方法可以识别井筒之间的共同分形模式,有助于确定地层单元的空间连续性。我们的方法能有效地探测地下地层的横向变化,将油井测井记录的断裂与不同流体存在下的各种过渡环境(如湖泊、浅海到河流)中的沉积模式联系起来。石炭系地层的分形维度最低,多分形性较弱。该研究利用分形分析改进地层相关性,加强地下特征描述和储层划分,尤其是在复杂地质环境中,并提高可靠性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Chaotic behavior of geophysical logs for stratigraphic hiatuses: A case study from Upper Assam Shelf, India

Chaotic behavior of geophysical logs for stratigraphic hiatuses: A case study from Upper Assam Shelf, India

We propose a novel fractal analysis-assisted approach for stratigraphic characterization to understand the in-situ subsurface geology of hydrocarbon reservoirs. By employing correlation dimension and multifractal detrended fluctuation analysis, we quantify the self-similarity and long-range dependencies in the geophysical logs, reflecting the unique sedimentation processes inherent in the stratigraphic formations of the Bhogpara oil field in the Upper Assam basin. The fractal properties of the logs associated with various stratigraphic units are used to establish a fractal-based stratigraphic signature. The hierarchy of the studied formations, based on the correlation dimension ranging from 1.98 to 1.13, is follows as: Girujan > Tipam > Barail > Kopili > Prang > Narpuh > Lakadong-Therria. Furthermore, the spectrum width values, was found to range from 0.70 to 2.04, reflecting the spatial correlation, geological complexity, and heterogeneity inherent in each formation as: Kopili > Prang > Narpuh > Barail > Girujan > Tipam > Lakadong-Therria. This method identifies common fractal patterns between wellbores and aids in determining the spatial continuity of stratigraphic units. Our approach effectively detects lateral variations in subsurface formations, linking well log fractality with depositional patterns through various transitional environments, such as lacustrine to shallow marine to fluvial, in presence of different fluids. The petroliferous formation exhibits lowest fractal dimension and weak multifractality. The research utilizes fractal analysis to improve stratigraphic correlation, enhancing subsurface characterization and reservoir delineation, particularly in complex geological environments, and enhancing reliability.

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来源期刊
Journal of Asian Earth Sciences
Journal of Asian Earth Sciences 地学-地球科学综合
CiteScore
5.90
自引率
10.00%
发文量
324
审稿时长
71 days
期刊介绍: Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance. The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.
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