塔里木盆地构造成岩作用对超深层断控型碳酸盐岩储集体的控制作用
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    摘要:

    构造成岩作用(Structure diagenesis)是沉积学与构造地质学等学科交叉融合发展形成的概念,旨在研究构造背景下构造作用产物与成岩改造之间的相互关系。本文以塔里木盆地塔河油田和富满油田为例,在系统梳理与总结了前人近二十年来研究成果的基础上,提出了适用于超深层断控型碳酸盐岩研究的新思路。依据前人地震及构造研究成果,结合测井数据以及地质资料,在明确断裂与断裂破碎带两种构造产物特征的基础上阐明断控背景下构造成岩作用对储层发育规律及有效性的控制作用。①断裂具有横向分带和走向分段特征,即垂直断裂走向发育具有“核带”结构的断裂破碎带,地震上以串珠状反射特征为主,平行断裂走向可分为拉分段、挤压段和平移段。②研究区经历多种构造成岩作用,主要包括胶结作用、溶蚀作用和破裂作用。③断层核主要发育规模较大的洞穴型储层,部分洞穴被充填储集能力降低,随着向破碎带过渡储层为裂缝孔洞型、孔洞型或裂缝型,至围岩带,几乎不发育储层。溶蚀作用与破裂作用是成储的关键要素,而胶结作用破坏储层。胶结作用破坏早期形成的孔隙,堵塞流体通道。溶蚀作用与破裂作用对储层改造程度的差异致使不同断裂分段的储层发育特征不同,总体上,拉分段的构造成岩作用最强,储层规模及有效性最优,挤压段次之,平移段较差。

    Abstract:

    Structural diagenesis is an emerging interdisciplinary concept that integrates sedimentology and structural geology, focusing on the interplay between tectonic products and diagenetic alterations within tectonic settings. This paper, using the Tahe and Fuman Oilfields in the Tarim Basin as case studies, proposes innovative methodologies and concepts for the structural diagenesis of ultra-deep fault-controlled carbonate reservoirs. These proposals are based on a systematic review and synthesis of research findings accumulated over the past two decades. According to previous seismic and structural studies, integrated with well logging and geological data, this study clarifies the controlling effects of structure diagenesis on reservoir development and effectiveness within a fault-controlled setting. This is achieved by defining the characteristics of both faults and fault damage zones as distinct structural products. Faults exhibit transverse zonation and strike segmentation. Perpendicular to the fault strike, a fault damage zone develops with "core-damage zone" structure, primarily characterized by beaded seismic reflections. Parallel to the fault strike, segments are classified as releasing bend, restraining bend, and translation bend. The study area experienced multiple structural diagenesis, including cementation, dissolution and fracturing. Large-scale cave type reservoirs predominantly develop within the fault core, though partial cave filling reduces reservoir capacity. Transitioning into the surrounding damage zone, reservoirs become fracture-vug, vug, or fractured types. Within the wall rock, effective reservoirs are virtually absent. Dissolution and fracturing are the key factors for reservoir formation. Conversely, the cementation predominantly degrades reservoir quality. Cementation destroys pre-existing pore spaces and obstructs fluid pathways. Variations in the efficacy of dissolution and fracturing across different fault segments lead to distinct reservoir characteristics. Overall, releasing bend exhibits the most intense structure diagenesis modification, resulting in reservoirs with the largest scale and highest effectiveness. Restraining bend ranks second, while single fault yields the least favorable reservoirs.

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  • 收稿日期:2025-11-08
  • 最后修改日期:2025-12-29
  • 录用日期:2025-12-30
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