Control of lamination on bedding-parallel fractures in tight sandstone reservoirs: the seventh member of the upper Triassic Yanchang Formation in the Ordos Basin, China

IF 2 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Hao Lu, Song Cao, Shaoqun Dong, Wenya Lyu, Lianbo Zeng
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Abstract

Tight sandstone reservoirs have extremely low porosity and permeability. Bedding-parallel fractures (BPFs) contribute prominently to the storage and seepage capability. However, the distribution of BPFs is remarkably heterogeneous, impeding the prediction and modeling of sweet spots. BPFs are controlled fundamentally by laminations, which are widely distributed in lacustrine tight reservoirs and provide most weakness planes. Based on core and thin section data, BPFs of the upper Triassic Chang 7 tight oil reservoir are characterized microscopically. The lamination combination unit, which is defined by distinctive lamination assemblage and relatively stable lamination thickness and space, is utilized as a homogeneous unit to measure the density of lamination and related BPFs. The influence of laminations on BPFs is discussed further. Results show that most bedding-parallel fractures are unfilled, with apertures generally <40 μm, mainly <10 μm. Larger apertures correlate with low filling degrees. The distribution of BPFs is intricately controlled by lamination type, density, and thickness. (1) BPFs tend to develop along different types by a priority sequence which reflects their mechanical strength. The development degree of BPFs also depends on the mechanical contrast with adjacent laminations; (2) When controlled by a single type of lamination, the density of BPFs increases with lamination density under a turning point and then decreases; (3) BPFs prefer to develop along the thinner lamination and are usually inside it, while controlled by thick lamination, BPFs tend to extend along the edge. The change in the thickness of laminations leads to a change in the development position of BPFs, indicating that the position of the weak plane controls the development position of BPFs; (4) When multiple types of lamination coexist, the type and thickness of laminations jointly influence the development of BPFs. Plastic thin laminations are conducive to the development of BPFs, while brittle thick laminations are not conducive. When the thickness of the plastic lamination is close to or less than that of the brittle, the influence of lamination type dominates BPFs, while the thickness of the plastic laminations is much larger than the brittle, the influence of lamination thickness will dominate.
致密砂岩储层中层理对层理平行裂缝的控制:中国鄂尔多斯盆地上三叠统延长地层第七段
致密砂岩储层的孔隙度和渗透率极低。层理平行裂缝(BPFs)对储层的储存和渗流能力起着重要作用。然而,BPFs 的分布具有明显的异质性,阻碍了对甜点的预测和建模。BPF从根本上受到层理的控制,层理广泛分布于湖相致密储层中,提供了大部分薄弱平面。基于岩心和薄片数据,对上三叠统长 7 号致密油藏的 BPF 进行了微观描述。层状组合单元具有独特的层状组合和相对稳定的层状厚度和空间,被用作测量层状密度和相关 BPF 的均质单元。进一步讨论了层理对 BPF 的影响。结果表明,大多数与层理平行的裂缝是未填充的,孔径一般为 40 微米,主要为 10 微米。孔径越大,填充度越低。BPF 的分布受层压类型、密度和厚度的复杂控制。(1) BPFs 倾向于按优先顺序沿不同类型发展,这反映了它们的机械强度。BPF 的发展程度还取决于与相邻层压板的机械对比;(2)当受单一类型层压板的控制时,BPF 的密度会随着层压板密度的增加而增加,直到一个转折点,然后再减小;(3)BPF 更倾向于沿着较薄的层压板发展,通常位于其内部,而受厚层压板的控制时,BPF 则倾向于沿着边缘延伸。层压板厚度的变化会导致 BPF 发展位置的变化,这表明薄弱面的位置控制着 BPF 的发展位置;(4)当多种层压板共存时,层压板的类型和厚度会共同影响 BPF 的发展。塑性薄层有利于 BPF 的发展,而脆性厚层则不利于 BPF 的发展。当塑料层压板的厚度接近或小于脆性层压板的厚度时,层压板类型对 BPFs 的影响占主导地位,而当塑料层压板的厚度远大于脆性层压板的厚度时,层压板厚度的影响将占主导地位。
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来源期刊
Frontiers in Earth Science
Frontiers in Earth Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
3.50
自引率
10.30%
发文量
2076
审稿时长
12 weeks
期刊介绍: Frontiers in Earth Science is an open-access journal that aims to bring together and publish on a single platform the best research dedicated to our planet. This platform hosts the rapidly growing and continuously expanding domains in Earth Science, involving the lithosphere (including the geosciences spectrum), the hydrosphere (including marine geosciences and hydrology, complementing the existing Frontiers journal on Marine Science) and the atmosphere (including meteorology and climatology). As such, Frontiers in Earth Science focuses on the countless processes operating within and among the major spheres constituting our planet. In turn, the understanding of these processes provides the theoretical background to better use the available resources and to face the major environmental challenges (including earthquakes, tsunamis, eruptions, floods, landslides, climate changes, extreme meteorological events): this is where interdependent processes meet, requiring a holistic view to better live on and with our planet. The journal welcomes outstanding contributions in any domain of Earth Science. The open-access model developed by Frontiers offers a fast, efficient, timely and dynamic alternative to traditional publication formats. The journal has 20 specialty sections at the first tier, each acting as an independent journal with a full editorial board. The traditional peer-review process is adapted to guarantee fairness and efficiency using a thorough paperless process, with real-time author-reviewer-editor interactions, collaborative reviewer mandates to maximize quality, and reviewer disclosure after article acceptance. While maintaining a rigorous peer-review, this system allows for a process whereby accepted articles are published online on average 90 days after submission. General Commentary articles as well as Book Reviews in Frontiers in Earth Science are only accepted upon invitation.
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