中国珠江口盆地白云凹陷珠海地层混合过程三角洲的沉积特征及其对石油勘探的地质意义

Q1 Earth and Planetary Sciences
Xiaojun Xie , Wu Tang , Shangfeng Zhang , Rui Zhu , Dongxu Fan , Ran Li
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引用次数: 0

摘要

南海北部珠江口盆地白云凹陷的珠海地层是一个海洋三角洲,受河流、波浪和潮汐等多种水动力的影响,形成了一个混合过程三角洲。在这些作用力的共同影响下,珠海地层砂岩地层的分布模式和储层结构极为复杂。本文详细描述了在白云凹陷钻探的珠海地层岩心剖面,重点介绍了岩心剖面的岩性、沉积构造、特殊容器和沉积动力学。研究还总结了河流、波浪和潮汐控制的混合动力三角洲的特征,并探讨了这一混合动力三角洲对油气勘探的地质意义。研究显示,受河流控制的沉积主要由中-细砂岩组成,具有交错层理和平行层理。此外,还观察到冲刷填充结构和钟形或箱形天然伽马射线测井曲线(GR)。地震反射显示出较强的振幅和较高的连续性。另一方面,波控沉积主要由粉砂和细砂岩组成,具有冲刷、波状交叉层理、丰富的生物扰动以及锯齿状和漏斗状的伽马测井曲线。地震反射显示出中等振幅和较高的连续性。潮汐控制沉积的特征是泥岩、粉砂岩和细砂岩的薄夹层,以及脉状层理、波状复合层理、透镜状层理和双胶层。潮汐控制沉积的 GR 曲线呈尖锐或锯齿状的漏斗形,地震反射呈现中等振幅和连续性。受沉积古地理和海平面变化的影响,白云凹陷珠海地层沉积时期控制沉积的水动力特征在平面尺度上表现出明显的分带性。珠海地层北部以河流控制为主,局部受波浪影响,潮汐影响很小。在南部地区,潮汐作用变得越来越重要。就储层性质而言,与潮汐控制和河流控制储层相比,波浪控制储层的孔隙度和渗透率明显更高。潮汐控制储层的异质性较高,孔隙度和渗透率值范围较大。不同地点不同水动力的影响导致白云凹陷珠海地层海洋三角洲沉积物中砂体的大小、形态和物理性质存在显著差异。因此,沉积水动力的类型和强度成为优质油藏开发的主要控制因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sedimentary characteristics and geological significance of a mixed-process delta for petroleum exploration in the Zhuhai formation of the Baiyun Depression, Pearl River Mouth Basin, China
The Zhuhai Formation in the Baiyun Depression of the Pearl River Mouth Basin in the northern South China Sea is a marine delta influenced by multiple hydrodynamic forces, including rivers, waves, and tides, resulting in a mixed-process delta. As a result of the combined effects of these forces, the distribution patterns and reservoir structures in the sandstone formations of the Zhuhai Formation are extremely complex. This paper provides a detailed description of the coring section of the Zhuhai Formation drilled in the Baiyun Depression, focusing on the lithology, sedimentary structure, special containers, and depositional dynamics of the coring section. It also summarizes the characteristics of a hybrid power delta controlled by rivers, waves, and tides, and explores the geological significance of this mixed-process delta for oil and gas exploration. The study reveals that sedimentation controlled by rivers primarily consists of medium-to-fine sandstones with interbedded cross-bedding and parallel bedding. Scour-fill structures and a bell or box-shaped natural gamma ray logging curve (GR) are also observed. Seismic reflection exhibits strong amplitude and high continuity. Wave-controlled sedimentation, on the other hand, predominantly consists of silt and fine sandstones with scouring, wave-formed cross-bedding, abundant bioturbation, and a serrated and funnel-shaped GR curve. Seismic reflection shows medium amplitude and high continuity. Tidally-controlled deposits are characterized by thin interbeds of mudstone, siltstone, and fine sandstone, as well as vein laminations, undulating composite laminations, lenticular laminations, and biclastic layers. The GR curves for tidally-controlled deposits are sharp or jagged with funnel shapes, and seismic reflections exhibit medium amplitude and continuity. The hydrodynamic features controlling sedimentation during the depositional period of the Zhuhai Formation in the Baiyun Depression exhibit evident zonation on a planar scale, influenced by sedimentary paleogeography and sea-level changes. River control is predominant in the northern Zhuhai Formation, with local wave influence and minimal tidal influence. In the southern part, tidal action becomes increasingly important. In terms of reservoir properties, wave-controlled reservoirs display significantly better porosity and permeability compared to tidally-controlled and river-controlled reservoirs. Tidally-controlled reservoirs exhibit high heterogeneity with a wide range of porosity and permeability values. The varying influences of different hydrodynamic drivers in different locations have led to significant variations in the size, morphology, and physical properties of sand bodies within the marine delta sediments of the Zhuhai Formation in the Baiyun Depression. Thus, the type and intensity of sedimentary hydrodynamics become the primary controlling factors for the development of high-quality reservoirs.
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来源期刊
Petroleum Research
Petroleum Research Earth and Planetary Sciences-Geology
CiteScore
7.10
自引率
0.00%
发文量
90
审稿时长
35 weeks
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