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A preliminary study on sedimentary mode of Putaohua Oil Layer in the East of Sanzhao Depression

机译:三昭抑郁症东部普陀油层沉积模式初步研究

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Based on ten well cores, seventeen hundred logging data and initial potential data, sedimentary characteristics and mode of shallow lacustrine fluvial-dominated delta of Putaohua oil layer in the east of Sanzhao depression were analyzed. It is realized that distributary channel sandbodies as sand body framework of this delta system, which is abundant, closely and narrow, and the framework of sand body is in a large number of narrow banded shape (mostly 200~300m), and can extend hundreds of kilometers of continuous, dense, overall was SW, and combines well with other types sand surface to become a better distributary channel sand body. Based on understanding of sedimentary background, developmental process, sedimentary characteristics and sedimentary facies type of Putaohua oil layer in Sanzhao depression, sedimentary mode of shallow lacustrine fluvial-dominated delta is established in the study area, and sedimentary mode of five subfacies is further divided: Delta distributary plain subfacies is mode of fluvial-dominated belt body; Transition region of front-distributary plain is mode of inshore; Inner front is mode of fluvial-dominated belt body; Transition region of inner front-outer front is mode of fluvial-dominated sheet sand; Shallow lacustrine fluvial-dominated delta outer front is mode of tide-dominated sheet sand; Also pointed out that overall shows NE-SW trending submerged distributary channel sandbodies which is abundant, closely and narrow is the main reservoir of the study area. It provides the solid geological basis for the establishment of spatial distribution pattern of reservoir; identify the causes of mainly monosandbody and further tapping the potential of oil field.
机译:根据TE以及核,1700个测井数据和初始潜在的数据,沉积特征和三肇凹陷东部葡萄花油层浅水湖泊河流控三角洲的模式进行了分析。应认识到,分流通道砂作为此增量系统的砂体框架,它是丰富的,密切和缩小,和砂体的框架是在大量窄带状形状的(主要是200〜300米),并能延长数百的连续的,致密的公里,整体为SW,并且很好与其它类型的砂面结合,成为更好的分流通道砂体。基于沉积背景,发展过程,沉积特征和沉积相的认识键入三肇凹陷葡萄花油层,浅水湖泊河流控三角洲沉积模式是建立在研究区,和五个亚相沉​​积模式又分为:三角洲分流平原亚相是河流主导皮带本体的模式;前分流平原的过渡区是近海的模式;内前是河流主导皮带本体的模式;内前部外前的过渡区域是河流主导片砂的模式;浅湖河流控三角洲外前是潮控片砂的模式;还指出,总体示出了NE-SW向的水下分流通道砂是丰富,密切和缩小是研究区的主储液器。它提供了建立储存器的空间分布图案的固体地质基础;确定单砂体为主,进一步的原因攻牙油领域的潜力。

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