Oolite beach carbonate reservoir of Feixianguan Formation in Luojiazhai, NW Sichuan Basin is a platform edge facies sediment with massive thickness and uniform distribution.
川东北地区罗家寨飞仙关组鲕滩储集层为碳酸盐岩台地边缘相沉积,具有厚度大、分布稳定的特点。
This paper has divided the sedimentary facies of Feixianguan Formation , and analyzed the distribution of oolitic limestone beach body.
本文进行了飞仙关组沉积相的划分与鲕粒灰岩滩体分布的分析。
Category and distribution of mangrove, and formation mechanism of the beach in which mangrove grew were introduced.
介绍了红树林的种类、分布及红树林海滩的形成机理和特点。
The main response feature of the bar-lagoon beach profile's was formation of secondary bars at mid tide zone.
沙坝-泻湖型沙滩剖面冲淤变化的主要特征是中潮带形成次一级沙坝。
The main response feature of the bar-lagoon beach profile was the formation of secondary bars at the mid tide zone.
沙坝-泻湖型沙滩剖面冲淤变化的主要特征是中潮带形成次一级沙坝。
The results show that the self-organized processes between the sediment, topography and swash can induce the formation of beach cusps.
结果表明滩角的形成过程具有自组织特征,因此滩角可以通过海滩泥沙、地形与波、流的自组织过程形成。
The major reservoir rock of the gas reservoirs in Member-2 of Jialingjiang Formation, Lower Triassic, at Hebaochang-Jieshichang region, is the dolomite with pinpoint pores, belonging to beach facies.
荷包场-界市场地区下三叠统嘉陵江组嘉二段气藏的主要储集岩为针孔白云岩,属海滩岩相。
It is a new problem to identify the oolitic beach reservoirs of Feixianguan Formation in East Sichuan by log data.
应用测井资料识别川东飞仙关组鲕滩储层是个新课题。
This paper gives demonstration to the cause of formation of beach and process of getting worse, as well as the conservaney work taken on.
文章论证浅滩形成及不断恶化的原因及所采取的疏浚维护措施;
The oolite beach of the lower Triassic Feixianguan Formation in eastern Sichuan basin developed in themargin of carbonate platform, and platform margins are always related to ocean trough.
四川盆地东部下三叠统飞仙关组鲕滩主要发育在碳酸盐岩台缘带上,而台缘带与海槽密切相关,找到了海槽就意味着找到了鲕滩。
Guan Jiapu area beach sea oil field main oil-bearing formation location whether last the third take town group, Guantao group and lay the third Shahe street group tomorrow.
关家堡地区滩海油田主要含油层位是上第三系明化镇组、馆陶组和下第三系沙河街组。
The shore-shallow lake and hemi-deep-deep lake develop in the first and second member of Nenjiang formation, and thin bed beach sands distribute fragmentarily.
嫩一段和嫩二段主要发育滨—浅湖和半深—深湖沉积,零星分布薄层砂滩砂体。
The shore-shallow lake and hemi-deep-deep lake develop in the first and second member of Nenjiang formation, and thin bed beach sands distribute fragmentarily.
嫩一段和嫩二段主要发育滨—浅湖和半深—深湖沉积,零星分布薄层砂滩砂体。
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