湖滩

基本解释 (translations)

lakeshore

与湖滩相关的网络例句 [注：此内容来源于网络，仅供参考]

The shallowest of the lakes, it can be pale as glass, and as smooth. Then a few hours later it can be insensately churning[4] under a fugitive sky. Its shores are low-lying, its beaches are narrow, but it is succulently pastoral.

它的湖水在五大湖中最浅，有时如玻璃清澈透明、平如镜面，可是几小时以后，在不可捉摸的天空下卷起无情的巨浪，伊利湖岸低矮，湖滩狭窄，但沿岸却一派田园风光，情趣盎然。

But Portage's beach, which opened last year, is the first step in an effort to reclaim the lakefront.

但是波蒂奇市的湖滩已经于去年向公众开放，是迈向湖滨利用的第一步。

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。

Qaidam basin ; Tertiary ; shore\|lake and shallow\|lake subfacies ; lake delta facies

柴达木盆地；第三系；滨—浅湖滩坝亚相；湖泊三角洲相

A comprehensive study on petrology, structures, facies models, facies associations and sedimentary systems in this paper shows that the main facies in Tertiary are shore-lake and shallow-lake subfacies, and lake delta facies from low-Gancaigou formation to low-Youshashan formation.

对该地区的地面、井下岩性和岩相进一步研究表明，自下干柴沟组至下油砂山组的储集砂体主要为滨一浅湖滩坝亚相和湖泊白三角洲相。

The Es formation was divided into seven third order sequences based on the seismic, drilling and logging data, and plans deposition system plane distribution maps of different time were plotted by dominance phase principle. The lower Es4 is flood-overlake facies mainly; the upper Es4 is meandering stream and braided river delta deposition above the shore shallow lake background; in the Es3 period, the south mainly developed braided river, meandering stream delta, the northeast area main developed meandering stream delta, the middle area mainly developed semi-deep lakean d deep lake sediments. From lower Es3 to upper Es3, the delta scale gradually increased and the depositional area gradually moved to the east and the southeast; the Es2 period was dominated by shore-shallow lake sediments and widely developed braided river delta and delta deposits; the Es1 period was dominated by shore-shallow lake shoal deposits, and in the south developed meandering stream and braided river delta deposits.The lothological traps of the Shahejie group are mainly fluxoturbidite and stratum lateral pinch-out, and its formation and the distribution of the lothological trap were controlled mainly by the basin structure characteristic, palaeogeomorphology and tectonic activity and so on. It had a beneficial geological condition to develope sublacustrine slump turbidite fans in Jishan, Jiangjiadian and Wawu.

利用地震、钻井、测井等资料，将古近系沙河街组划分出7个三级层序，通过剖面沉积学分析，以优势相原则绘制不同时期各亚段沉积体系平面分布图：沙四下总体以洪水-漫湖沉积为特征，沙四上沉积时期是在滨浅湖背景之上发育了曲流河三角洲和辫状河三角洲沉积；沙三段沉积时期南部主要发育辫状河、曲流河三角洲，西北部地区发育曲流河三角洲，中部地区主要为深湖—半深湖沉积；由沙三下至沙三上，西北部三角洲规模逐渐增大，沉积范围逐渐向东、东南方向推进；沙二段沉积时期为滨浅湖沉积，在背景之上广泛发育了辫状河三角洲和三角洲沉积；沙一段以滨浅湖滩坝沉积为特征，南部发育了曲流河三角洲和辫状河三角洲沉积；沉积地层中的岩性圈闭以滑塌浊积岩岩性圈闭和地层侧向尖灭型岩性圈闭为主，其形成和分布主要受盆地结构、沉积古地貌和构造活动强度等因素控制，北部基山、南部江家店和瓦屋具有发育滑塌浊积扇的良好地质条件。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1～N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

进一步研究了本区碎屑岩储层的岩石学特征、成岩作用特征、物性特征，研究认为该区储集体类型有分流河道砂体、分支河道砂体、河口坝、远砂坝、席状砂砂体、滨湖砂滩、浅湖砂坝砂体及灰坪；N1层属于低孔、特低渗储层，孔隙类型以原生、次生粒间溶孔为主；分析了影响储层物性的因素主要为沉积作用、胶结作用、溶蚀作用和构造破裂作用；进行了储层评价与有利相带预测，将储层分为三类并划分了有利区带、较有利区带，认为Ⅶ号断层以东的辫状河三角洲前缘亚相和部分浅湖亚相是N1的有利储集相带，储层以Ⅰ、Ⅱ类为主。

But waterfront became victim for construction of city and exploitation of oil during oil city was developed.So some problems occurred such as pollution of water,desertification of lake shoal,decreased water area and destroyed ecosystem of water area.

然而在油城发展的历程中，滨水资源成为了城市建设和石油资源开发的牺牲品，导致水体污染、湖滩荒漠化、水体面积减少、水域生态系统破坏等现象发生。

In the Eogene and Neogene, Qaidam Basin experienced the multiphase tectonic movement; the paleoclimate evolved from warm-humid to arid; the water in the basin was gradually salinized; the depocenter migrated from west to east. The master factors and developmental characters of lithologic hydrocarbon reservoirs have their own particularity. Taking the fine exploration zones of the southwest hydrocarbon-rich depression in Qaidam as the key point, with the analysis of source-rock distribution, sedimentary evolution and sedimentary system distribution, the author proposes that the density difference increases after the fluvial water enters, then clam and bar sand bodies are formed easily due to density flow. Highstand system tract and transgressive system tract below the maximum flooding surface are the main exploration areas of lithologic reservoir.

柴达木盆地古近纪－新近纪经历了多期构造运动，古气候由温湿向干旱演变、湖盆逐渐咸化、沉积中心由西向东迁移的演化过程，地层岩性油气藏的主控因素和发育特征有其特殊规律，以柴达木盆地柴西南富油气凹陷精细勘探区带为重点，通过分析烃源岩展布、沉积演化和主要沉积体系展布，提出咸化湖盆在河流入湖后因密度差较大，易形成密度流等成因的各类滩坝砂体，最大湖泛面之下的高位体系域、湖侵体系域是地层岩性油气藏的主要勘探领域。

The study results show that:①The distribution of Cd in shallow surface soils is characterized as: The content of Cd in lacustrine deposit, alluvial lacustrine and alluvial-diluvial low-lying plain is 1.4 to 1.8 times as high as in alluvial-diluvial high valley flat and alluvial-diluvial high bank physiognomy areas.②The content variation of Cd in horizontal distribution was controlled by clay primarily and OrgC secondly. The variation of OrgC was major factor that affected the content variation of Cd in vertical distribution.

结果表明：①研究区浅层土壤中w的分布特征为，湖积低平原区、冲－湖积低平原区及冲洪积低洼平原区地貌成因类型土壤中的含量明显高于冲洪积高漫滩平原区、冲洪积高亢平原区地貌成因类型土壤，其质量分数差异达1.4~1.8倍；②研究区不同地貌成因类型土壤中，w的横向分布特征主要受黏粒含量分布的控制，其次是wC(下标 org；垂向分布特征的主要控制因素是wC

与湖滩相关的网络解释 [注：此内容来源于网络，仅供参考]

bev：是,就是;表示,意味着;等于;成为;在

bayn.(海或湖泊的)湾;山脉的低凹处 | bev.是,就是;表示,意味着;等于;成为;在 | beachn.海滩,湖滩,河滩

lacustrine clay：湖成粘土

lacustrine beach 湖滩 | lacustrine clay 湖成粘土 | lacustrine deposit 湖沉积,湖相沉积

lagoon：舄湖

(2)潟湖(lagoon) 指被沙坝(半)封闭的坝后水域:即小海. 小海面积达49km2,这在华南沿海众多沙坝-潟湖体系中,是很突出的. 但湖水很浅,多在1m左右. 潟湖的另一特点是湖岸周围有泥质潮滩(tidal flat)存在, 这些潮滩随涨、落潮时而淹没或出露. ......

littoral deposit：沿岸沉积;海滩沉积地;湖滩沉积地

litter container with cowl 有通风罩废物箱 | littoral deposit 沿岸沉积;海滩沉积地;湖滩沉积地 | live application 登记在轮候册上的有效申请

mudbank：(河、湖或海边的)泥滩

downward enrichment 次生富集 | mudbank (河、湖或海边的)泥滩 | veralozidine 藜芦兹定

oxbow lake：牛轭湖

一些旧河道里仍然还有水,这被称为牛轭湖(oxbow lake). [译注:1.漫滩,大型洪水时期会被淹没的一片土地;2.牛轭湖,当河流弯曲过大时,河流会在弯曲处改变航道,在原河弯曲处留下的就是牛轭湖]在过去1万年里,密西西比河大约每一千年就会沿着200英里长的海岸线蜿蜒,

oxbow lake deposit：牛轭湖沉积

如一个完整的韵律可以包括下部的河床沉积(stream bed deposit)、中部的河漫滩沉积(flood basin deposit)及上部的牛轭湖沉积(oxbow lake deposit). 这样一个韵律代表了河床在一次侧向摆动时逐次沉积的产物. 如河床反复进行侧向摆动,

sea-horse breakers：海马滩

sea scan|海上扫描 | sea-horse breakers|海马滩 | seaforth , l . |锡福斯湖

fluviatile lake：河成湖;活水湖;河中湖

fluviatile flood-plain 河漫滩 | fluviatile lake 河成湖;活水湖;河中湖 | fluviatile sediment 河流沉积

fluviatile lake：河成湖

河漫滩 fluviatile flood-plain | 河成湖 fluviatile lake | 河流沈积 fluviatile sediment