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Characterization and discrimination of paleokarst breccias and pseudobreccias in carbonate rocks: Insight from Ordovician strata in the northern Tarim Basin, China

机译:碳酸盐岩中古岩溶角砾岩和假角砾岩的特征与判别:塔里木盆地北部奥陶纪地层的认识

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Ordovician carbonates in the central and southern Halahatang area of the Tarim Basin host highly productive hydrocarbon reservoirs. Previous studies suggest that the Yingshan and Yijianfang Formations (the primary producing intervals) have been extensively karstified. However, the current author has not observed significant karst features in the formations based on the detailed study of 380 m long cores from 16 wells. In the current study, true breccias are only identified in two wells in the Lianglitage Formation, including crackle and mosaic breccias as well as chaotic, clast-supported breccias. The breccias are interpreted as karst-related breccias that formed in near-surface environments during pre-Silurian subaerial exposure, and timing of karstification probably coincided with eustatic sea-level fall caused by the middle Katian glaciation. Widespread "karst features" of the Yijianfang and Yingshan Formations identified as breccias or sediment-filled cavities in many previous studies are actually only a mottled fabric (pseudobreccia) caused by selective diagenetic alteration and infiltration of bitumen in the deeper subsurface. The color difference between pseudoclasts and pseudomatrix does not reflect a mixture of clasts and cave sediments, but instead is characterized by distinct, nevertheless commonly subtle, variations in the limestone texture and whether bitumen is present. One the basis of core and thin section observations, SEM (scanning electron microscope) and XRD (X-ray diffraction) analyses, the author presents criteria to distinguish karst breccias and pseudobreccias that can be applied to other similar carbonate deposits. Discrimination between karst breccias and nodular limestones is also presented. Differentiation of karst and pseudokarst features serves not only an academic interest, but also has important applications for the exploration and development of carbonate reservoirs. (C) 2019 Elsevier B.V. All rights reserved.
机译:塔里木盆地中部和南部哈拉哈当地区的奥陶系碳酸盐岩拥有高产的油气藏。先前的研究表明,影山组和宜建坊组(主要的生产区间)已被广泛地岩溶化。但是,根据对16口井380 m长岩心的详细研究,目前作者尚未观察到岩层中明显的岩溶特征。在当前的研究中,仅在良里塔格组的两口井中才发现了真实的角砾岩,包括裂纹和镶嵌角砾岩以及混乱的,由裂口支撑的角砾岩。角砾岩被解释为与-六里王前陆上接触期间在近地表环境中形成的与喀斯特有关的角砾岩,而喀斯特地化的时机可能与凯蒂中期冰川作用引起的海平面喜人下降有关。在先前的许多研究中,易建房组和应山组的广泛的“岩溶特征”被识别为角砾岩或充满沉积物的空腔,实际上只是由深部地下的选择性成岩作用和沥青渗透引起的斑驳的构造(伪角砾岩)。伪碎屑和伪基质之间的色差不能反映出碎屑和溶洞沉积物的混合,而是以石灰石质地以及是否存在沥青为特征,尽管如此,但通常是细微的变化。作为岩心和薄层观测的基础,SEM(扫描电子显微镜)和XRD(X射线衍射)分析,作者提出了区分可用于其他类似碳酸盐矿床的岩溶角砾岩和假角砾岩的标准。还介绍了岩溶角砾岩和节状石灰岩之间的区别。岩溶和假岩溶特征的区分不仅具有学术意义,而且对碳酸盐岩储层的勘探和开发具有重要的应用价值。 (C)2019 Elsevier B.V.保留所有权利。

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