您要查找的是不是：
- sedimentary facies association 沉积相组合
- The orebearing sequence is littoral-lagoon sedimentary facies. 层状、似层状铝土矿规模大、品位高,主要分布于豫西地区;
- Compiling sedimentary facies maps, compiling digenetic facies maps and... 预测的3块有利储集层分布区与实际钻探结果十分吻合。
- By means of subdivision of sedimentary facies, determination of oil reservo... 该思路、方法对复杂地质条件下的精细油层评价具有一定借鉴。
- From Paleocene to Miocene, the sedimentary facies evolved from the extensive alluvial fan to the braided fluvial river environment. 从古新世到中新世，柴达木盆地北缘经历了由大规模冲积扇沉积到辫状河沉积的演化过程。
- There are two types of sedimentary facies in this region: the alluvial fan and the braided fluvial river. 结绿素－红山地区古新统至中新统发育2种沉积相类型，即冲积扇和辫状河。
- The sedimentary systems and facies associations of Huangxian Formation were studied with the help of principles and methodolohy of basin analysis. 本文采用盆地分析的基本原理和方法,对黄县盆地的沉积体系与相构成进行了研究。
- Major sedimentary facies in the Luohe Formation include alluvial fans facies, eolian facies,braided fluvial facies, and desert facies. 洛河组主要沉积了冲积扇相、风成沉积相、辫状河相和沙漠相;
- Sand bar sub-facies of lagoon, front delta, sheet sandstone of offshore sea are the best sedimentary facies belts for the oil &gas accumulation. 泻湖相堡坝亚相、三角洲相前缘亚相以及滨海相席状砂亚相是砂岩储层分布和发育的最有利相带。
- It is the first time to apply this method to study sedimentary facies of the Paleocene-Miocene in the Qaidam Basin. 这是首次将定量的沉积相研究方法应用于柴达木盆地的古新统至中新统。
- The sedimentary facies relating with carbonate rock include lakeshore, bank, bank margin, bathyal lake subfacies. 生物浅滩具有分布范围广阔、顶面平坦、进积迅速、前斜坡明显、沉积旋回发育、沉积厚度较小但稳定的特征。
- The reservoir physical property were primarily dominated by sedimentary facies、corrosion and dolomization. 储集物性主要受沈积相带及溶蚀和白云岩化作用的控制。
- The sedimentary facies are mainly fluvial facies,shallow lacustrine and coastal facies. 隆起区为河流沉积区，边缘为滨浅湖及河流交替沉积。
- The development of the reservoir is controlled by sedimentary facies, dolomitization, corrosion and fractures. 储层为低孔低渗性裂缝-孔隙型，发育程度主要受沉积相、白云石化作用、溶蚀作用和裂缝控制；
- They formed in continental faulting basins and their sedimentary facies mainly include river, delta and fan delta. 其形成环境主要为陆相断陷盆地的河流、三角洲和扇三角洲。
- The main sedimentary facies are carbonate plateform edge,open carbonate platform and limited carbonate platform. 沉积环境以台地边缘、开阔台地相、局限台地相为主；
- Reservoir porosity is mainly influenced and controlled by sedimentary facies and diagenesis. 储层孔隙度主要受沉积相和成岩作用的影响和控制。
- The sedimentary facies includes alluvial fan, fan-delta, offshore lake, shallow lake and deep lake facies. 沉积相类型包括：冲积扇相、扇三角洲相、滨湖相、浅湖相、深湖相。
- Different sedimentary facies with different lithofacies formed in different stages of basin development. 不同的沉积相类型出现在盆地发育的不同阶段，并由不同的岩石相构成。
- Carbonate sedimentary facies show a strong migration trend from southwest to northeast. 碳酸盐岩沉积相表现出很强的由西南向东北的迁移性。
