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Home > chinese-english > "river mouth bar" in English

English translation for "river mouth bar"

河口坝
河口沙坝
河口沙洲
拦江沙
拦门沙


Related Translations:
mouth piece:  传话机接口管口承送话口,泵吸口,封口件吸口
small mouth:  小口
mouth open:  张口位张着嘴
mouth to mouth method:  口吸法
mouth brush:  口刷
mouth cavity:  口腔
mouth adapte:  口用麻醉接头
mouth width:  嘴巴宽度
wave mouth:  波状齿
fish mouth:  鳄鱼嘴
Example Sentences:
1.According to synthesize evaluate , the distributary channel sandbodies and river mouth bars are best reservoir
通过综合评价认为,水下分流河道和河口砂坝微相为本区最好的储集层。
2.The delta front mainly developed in chang 6 , which includes microfacies , such as distributary channel sandbodies , river mouth bars , distal bars and so on
长6期是三角洲建设的高峰期,发育三角洲水下分流河道与河口砂坝砂体及远砂坝微相。
3.According to analysis of sedimentology , we think the most benefit environment to reservoir is under - water branch and river mouth bars microfacies , which often form thick sand bodies of high porosity of permeability
从沉积相分析认为,有利于储层发育的沉积环境是水下分流河道和河口砂坝微相,水下分流河道控制了砂体的走向及分布区。
4.According to observing the core and well logging facies analysis , yanchang 4 + 5 sector to yangchang 3 mainly developed underwater distributary channel , river mouth bars , underwater natural levee , underwater crevasse splay , interdistributary bay , far bars , etc . and some shallow lake subfacies
根据岩芯观察以及测井相分析,认为长4 + 5 ?长3期以水下分流河道、河口砂坝、水下天然堤、水下决口扇、分流间湾和远砂坝等沉积微相以及部分浅湖亚相沉积为主。
5.Yanchang 4 + 5 sector to yanchang 3 sector lithofacies palaeogeography pattern was stable , because the constitution background was steady , and the source direction had no change , and supply was abundant . in those sectors the basin development was in lake retreat , and in the period of extinction gradually , and formatted construction delta deposit , but in yanchang 33 period the sedimentary speed were greater than construction speed , showing that overriding river mouth bars were abundant
长4 + 5 ?长3期湖盆发展处于湖退、萎缩逐渐消亡时期,由于构造背景稳定,物源来源方向没有变化,物源供给充分,所以岩相古地理格局基本一致,形成建设性三角洲沉积,但长3 ~ 3期沉积速率大于构造沉降速率,表现为叠置河口砂坝极其发育。
6.The most favorable reservoirs of study formatioms in study area are delta river mouth bar sand body and sublacustrine fan sand body . the sublacustrine fan sand body region developed in each sand group and the river mouth bar sand body region developed in gao 5 sand - group are the most favorable regions of developing lithologic traps
研究区研究层段的最有利储层是三角洲河口坝砂体和湖底扇砂体,各砂组发育的湖底扇砂体区和高5砂组发育的河口坝砂体发育区是形成岩性圈闭最有利的场所。
7.According to the abundance well logging , mud logging and core analysis data , gaotaizi reservoir has been classified into four sand group with the principle of cycle comparison and classified control . based on the detailed study of lithologic character , sedimentary structure , paleontologic fossils , depositional sequence , rock association and logging data , the microfacies of the studied area are divided into such seven types : subaqueous distributary channel microfacies ; river mouth bar microfacies ; subaqueous interdistributary channel microfacies ; subaqueous crevasse channel microfacies ; subaqueous natural barrier microfacies ; distal bar microfacies ; delta front sheet sand microfacies . the characteristic of each sedimentary microfacies are described detailedly
通过研究大量测井、录井资料和岩芯资料,依据“旋回对比,分级控制”的原则,把研究区高台子油层划分为g 、 g 、 g 、 g四个砂层组。通过对研究区岩性、沉积构造、古生物、沉积序列、岩石组合及测井曲线特征进行研究的基础上,认为研究区高台子油层属于三角洲前缘亚相沉积,并将研究区沉积微相划分为:水下分流河道、河口坝、水下分流河道间、水下决口扇、水下天然堤、远砂坝、席状砂等七种微相类型。
8.Using sedimentary facies analytical and formation inverse technique , the depositional characteristics and distribution of dujiatai formation of this area were described , disclosing that delta front facies and prodelta facies were mainly developed in dujiatai formation . material source are mainly from southern and northeast of the working area . sand types are mainly of delta front subwater distributaries channel sand body , river mouth bar and sheet sand body with large degree of planar variation
2 .采用沉积相分析及储层反演预测技术,对新齐14井区杜家台油层储层沉积特征及展布特征进行了详细描述,揭示出本区主要目的层杜家台油层属t -扇二角洲沉积,发育扇三角洲前缘亚相及前扇三角洲亚相,物源主要来自于工区南部及东北部,发育的砂体类型土要为扇三角洲前缘水下分流河道砂体、河口坝砂体及席状砂砂体。
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