沉积结构 meaning in Chinese
depositional fabric
depositional texture
depositionalfabric
sedimentary texture
Examples
- Sediment microfacies , micro - construction , the variation iri sandbody rhythm and structures , and micro - pore configuration non - uniformity are main factors that affect or control the forming of remaining oil and its distribution in different scale reservoir rock
沉积微相、微构造的变化、砂体不同韵律性及沉积结构的变化、以及微观孔隙系统的非均质性等是控制和影响不同规模储层中剩余油形成和分布的重要因素。 - The fluvial , delta , and lacustrine sedimentary system was realized according to the analysis of the fossils , sedimentary structure , sedimentary cycle , rhythmic bedding and other criteria in the yanchang formation . the sedimentary microfacies of the chang - 6 oil - bearing beds was identified through its fine description , and the evolution of palaeogeography was revealed
通过古生物、沉积结构与构造、沉积韵律、沉积厚度与沉积旋回特征和测井相分析等，在延长组中识别出河流、三角洲、湖泊沉积体系，以及长6油层组的沉积微相，并对长6油层组各小层的沉积微相进行了精细描述，反演出其古地理的演化历程。 - The occurrence ofland crack is the results of the asymmetry land subsidence . therefore , application the 3stechnology in studying these problems is a realistic and tough matter for expertise . recently gis as a newly - developed technology for dealing and storing spatialinformation has been wildly used in a various fields , geology field without exception
论文重点研究了arcgis平台下基岩构造模型、第四纪沉积结构模型、地下水含水系统结构模型的三维可视化实现方法,并利用comgis在通用开发环境下嵌入了gis功能;在ao的二次开发研究中,利用activex技术实现了3s数据信息在arcgis环境中的无缝结合。 - Based on the detailed research on the sedimentary rocks of northwest ordos basin in their textures , structures , vertical sequences and logging response , six kinds of sedimentary facies can be recognized in this work , i . e . , alluvial fan , stream , fan delta , braided delta , delta , lake , barrier beach and carbonate platform , respectively , and more detailed classification of sedimentary subfacies and microfacies for each sedimentary facies are also made in the work
本文通过对鄂尔多斯盆地西北部沉积岩沉积结构、沉积构造、垂向序列及测井响应的深入研究，识别出冲积扇、河流、扇三角洲、辫状河三角洲、曲流河三角洲、湖泊、障壁海岸及碳酸盐台地等8种沉积相类型。在此基础上，对每一种沉积相又进行了详细的沉积亚相和微相的划分。 - Based on the direction of sources and the ratios of sandstone to formation of sedimentary rocks , together with the sedimentary structures and textures , paleocurrent direction and the characteristics of paleontology , etc . , the planimetric maps of sedimentary facies of each stages in the studied area are compiled in order to recognized the extension of dominant facies and the evlotionary history of sedimentary environment , hi the stage of benxi and taiyuan , lagoon - tidal flat sediments are widespread in the area , and the deposits of estuary , lagoon and small delta in the northwest margin of ordos
以物源方向和沉积岩砂地比值为基础，结合沉积结构构造、古水流方向及古生物特征等，编制了研究区各期次的沉积相平面图，以识别优势相展布和沉积环境演化。本溪期和太原期研究区泻湖?潮坪沉积分布广泛，西北缘发育河口湾、泻湖及小型三角洲沉积。