河流型浅水三角洲河流相砂体预测方法研究

Wang Lu
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引用次数: 0

摘要

浅湖盆河控三角洲前缘亚相砂体分布广泛,以砂体薄、规模小、多样化为主要特征,与经典三角洲沉积模式中的三角洲前缘发育大尺度、厚口砂坝沉积有较大区别。目前,其中大部分在开发的产油程度较差,是东部老油藏的主要靶区,对浅湖相河流主导的三角洲前缘亚相的单一砂体形成、展布特征和沉积模式的精细解剖和深入了解尤为迫切。以宋方屯油田南部永56-96区块为例,对几种砂体预测方法进行了分析比较,对研究区地震储层和地震储层进行了联合预测,有效识别了薄水道砂体和片状砂体。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Prediction Method of Fluvial Facies Sandbody in Fluvial Shallow Water Delta
Shallow lake basin fluvial-dominated delta front subfacies’s sandbody are widely distributed, and the thin sand body, small scale and diversification as the main features, and they are quite different from delta front in the classic delta sedimentary model developed large-scale and thick estuary sand dam sedimentary. At present, most of them in the development of the oil producing degree is poor, is the main target area in Eastern old oil reservoir, fine anatomy and in-depth understanding of shallow lacustrine fluvial-dominated delta front subfacies’s single sandbody formation, distribution characteristics and sedimentary model is particularly urgent. Taking Yong 56-96 block in the southern part of Song Fangtun oil field as an example, this paper analyzed and compared several prediction methods of sand bodies, and made joint prediction of seismic and seismic reservoirs in the study area, thus effectively identified thin channel sand bodies and sheeted sand bodies.
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