Control of differential tectonic activities on carbonate reservoirs in craton basin: A case study of the subsalt reservoir of Majiagou Formation in Ordos Basin
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摘要:
中国海相碳酸盐岩往往具有发育时期较老、埋藏较深、后期成岩作用改造较强等特点，致使对其优质碳酸盐岩储层及其主控因素的研究仍存在较大的进步空间。鄂尔多斯盆地马家沟组沉积时期，盆地由拉张动力背景向南北向挤压动力背景转换，从而诱发了一系列的构造活动。为了探讨不同构造活动对马家沟期马五段盐下沉积的影响，文章在前人研究基础上，以碳酸盐岩沉积学为理论指导，对研究区内二维地震剖面进行剖析，总结差异性构造活动，分析马五段盐下沉积期地震相与沉积相的特征，阐述差异性构造活动对颗粒滩储集体的影响，得到以下几点认识：（1）研究区识别出4种地震相类型，对应不同沉积相类型，其中颗粒滩储层为研究区内优势储集体；（2）盆地内发育基底断裂（拗拉槽）、同沉积断裂及古隆起3类构造活动；（3）将不同类型的构造活动与颗粒滩储集体进行匹配分析，总结出差异性构造活动对此类碳酸盐岩储集体的发育及分布的控制作用模式，并将颗粒滩储集体分为断控储集体和隆控储集体两大类。
Abstract:Carbonate rocks in China tend to have the characteristics of the older development period, deeper burial, and stronger later diagenetic transformation, which leaves a large space for the study of high-quality carbonate reservoirs and their main controlling factors in China. During the sedimentary period of Majiagou Formation in the Ordos Basin, the basin witnessed changing from tension to longitudinal compression, which induced a series of tectonic activities. To explore the influence of different tectonic activities on the subsalt deposition of Mawu Member in Majiagou Age, based on the previous studies and under the guidance of carbonate sedimentology, two-dimensional seismic profiles in the study area were analyzed, and differential tectonic activities were summarized. Combined with the analysis of seismic facies and sedimentary facies in the sub-salt sedimentary period of the Mawu Member, the influence of differential tectonic activities on the grain beach reservoir were depicted. As a result, the following understandings are obtained: a. four types of seismic facies have been identified in the study area, corresponding to different types of sedimentary facies, of which the grain beach facies is a good reservoir in the study area; b. there are three types of tectonic activities in the basin, basement faults (sag troughs), synsedimentary faults and uplifts; and c. based on the matching analysis of different types of tectonic activities and grain beach reservoirs, the control of differential structural activities on the development and distribution of this kind of carbonate reservoir is finally obtained, and its action mode is summarized. Finally, granular beach reservoirs are divided into fault-controlled reservoirs and uplift-controlled reservoirs.
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图 3 鄂尔多斯盆地马五段盐下沉积模式（据Fu et al., 2017）
Figure 3.
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