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characteristics of sedimentology
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  “characteristics of sedimentology”译为未确定词的双语例句
     This paper presented the sedimentation model of clastic rock reservoir of lake basin four fans, and outlined the principle characteristics of sedimentology and development.
     作者提出了湖益四扇储集层沉积模式,总结出组成湖盆四角两种基本相单元的沉积学特征及其开发地质学特征。
短句来源
     According to the characteristics of sedimentology and the analysis of the Fischer Plot, the cycles are formed in the upland systern domain of the 3rd order sequence and controlled by Milankovitch-induced high-frequency sea-level fluctuation.
     根据沉积学特征及Fischer图解分析,这些米级旋回形成在三级层序的高位体系域,受米兰柯维奇轨道参数诱导的高频海平面变化所控制。
短句来源
     Based on a large number of data of core, log and seism, and by the newest methods of sedimentology, this paper clarified the characteristics of sedimentology of Shahezi Formation in Western Fault Basins Belt of North Songliao Basin.
     大量地震、录井、测井资料沉积学分析结果表明 ,松辽盆地北部西部断陷带沙河子组发育的沉积体系有扇三角洲、湖泊、湖底扇体系和火山岩 .
短句来源
     The characteristics of sedimentology and palaeontol_ ogy suggest that NCB was quite different from SCB in Proterozoic, but similar to the Siberia block.
     沉积学和古生物学特征表明元古宙华北陆块不同于华南陆块,而与西伯利亚陆块相似。
短句来源
     Based on a large amount of data of core, log and seism, and using the newest methods of sedimentology, this paper clarified the characteristics of sedimentology of Yingcheng Formation in western fault basins belt of North Songliao Basin.
     根据地震、录井、测井分析表明 ,松辽盆地北部的西部断陷带营城组发育的沉积体系有扇三角洲、湖泊、湖底扇和火山岩 ;
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     And the characteristics of the G.
     通过仿真和实验,也验证了G.
短句来源
     characteristics;
     三、发展的特点;
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     The characteristics of G.
     论文首先对语音编码的各种方案进行了比较,并对G.
短句来源
     The Study of Sedimentology and Reservoir Characteristics in Chagan Depression
     查干凹陷沉积与储层特征研究
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     Its characteristics include:
     它的特征有:(1).
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The characteristics of sedimentology and petrology of the Middle Cambrian in western Shandong province show that:(1)The oolitic sediments developed at various places and stratum of north China are almost the allogenic sediments,but not the original "shoal".They had been influenced by the changes of sea level and water current,so that the ooids was transported in a short or long distance.In the study area,the oolitic limestone are not formed at the same time,it is time transgressive(diachronons).In general,the...

The characteristics of sedimentology and petrology of the Middle Cambrian in western Shandong province show that:(1)The oolitic sediments developed at various places and stratum of north China are almost the allogenic sediments,but not the original "shoal".They had been influenced by the changes of sea level and water current,so that the ooids was transported in a short or long distance.In the study area,the oolitic limestone are not formed at the same time,it is time transgressive(diachronons).In general,the horizon of oolitic limestone elevated gradually from SE to NW.That is the magnafacies,not the parvafacies.(2)The different texture of ooids occurred in the same oolitic limestone bed or thin band may be caused by the mixing of ooids form different places,termed the "sedimentary mixing",or owing to the ooids affected by the different diagensis after deposit,termed the "diagenetic mixing".(3)Following the ooid deposit,the algal sediment composited of Epiphyton developed.They occurred at the tidal flat,that is the algal flat.The algal sediments interbeded with the ooid sediments occurred off and between algal flats,as a result of frequent changes of sea level and tidal current.(4)The ooids (mainly brick and radial texture) of the Zhangxia Formation lower member basically formed under the condition of stronger and medium active environment,the ooids (mainly arc texture) of the upper member basically fromed under the weaker active environments.(5)Before the Zhangxia Formation upper member and the Upper Cambrian Gushan Formation,the obvious depositonal break caused by the sea level falling had happened.(6)Summarizing the sedimentary environment can be induce out the distribution situation of sedimentary facies form near land to open sea.They are in turn:tidal(algal)flat facies near shore(ooid) sand sheet(or ridge)facies restricted water field(or lagoon)facies tida(ooid) bar facies open sea facies.

鲁西地区中寒武统张夏组岩石的各种沉积特征表明:①华北地区普遍发育的鲕粒沉积在许多地点和层位是受海平面和水流条件变化影响的异地沉积物,而并非原始的“滩”。不同地点的鲕粒沉积具穿时性,一般由东和南向西和北层位逐步抬高,而并非同一时间的产物,即它们属同性相,而非同时相;②在鲕层中不同结构的鲕粒在一起,是由于沉积过程中不同地方的鲕粒相混合造成的,可称“沉积混合”,有的是在沉积稳定后受差异成岩作用的影响而造成的,可称“成岩混合”;③鲕粒沉积之后普遍为一套藻沉积,基本组分是Eiphyton,,它处于潮坪环境,即藻坪。其中潮渠和干裂较发育。藻沉积的类型有藻斑块,藻丘、叠层石,个别地点发育藻礁;④由于海平面和潮流条件的频繁变化,使藻坪外或藻坪间的鲕粒沉积与藻坪沉积相互交替;⑤张夏组上、下段中鲕粒的形成环境不同,前者主要是较弱扰动条件下的产物,后者主要是较强和中等扰动条件下的产物;⑥综合沉积环境分析归纳出主要沉积相带的基本展布状况,由近陆向外海依次是:潮坪相—受局限水域(或泻湖)相—潮汐坝相—开阔浅海相。

The alluvial fan, fan delta, delta and underwater sandbody are the main reservoirs of interior basin in lake basin clastic rock sedimentary system. The formation and development of lake basin four fans are closely related with water current which is one of main transportation forces. The lake basin clastic rock sedimentation is composed of channel facies and non-channel facies. This paper presented the sedimentation model of clastic rock reservoir of lake basin four fans, and outlined the principle characteristics...

The alluvial fan, fan delta, delta and underwater sandbody are the main reservoirs of interior basin in lake basin clastic rock sedimentary system. The formation and development of lake basin four fans are closely related with water current which is one of main transportation forces. The lake basin clastic rock sedimentation is composed of channel facies and non-channel facies. This paper presented the sedimentation model of clastic rock reservoir of lake basin four fans, and outlined the principle characteristics of sedimentology and development. It is concluded that channel facies can be as main oil reservoir, while non-channel facies as remaining oil reservoir.

湖盆碎屑岩沉积体系中,冲积扇、扇三角洲、三角洲、水下角砂体是内陆盆地的主要油气储集体。湖盆四扇的形成和发展与水流作用密切相关,水流作用是主要搬运动力,贯穿于湖盆四扇沉积始末,湖盆碎屑岩沉积基本上都是由水道相和非水道相两种主要相单元构成,这两种基本相单元组成了湖盆四扇碎屑岩储集层沉积的骨架砂体。作者提出了湖益四扇储集层沉积模式,总结出组成湖盆四角两种基本相单元的沉积学特征及其开发地质学特征。水道相是开发的主力油层,非水道相是剩余油分布的主要层位。

Two kinds of meter-scale carbonate cycles are developed in the Bioclastic Limectone Member of the Bachu Formation in the Lower Carboniferous of the Tarim Basin, i. e. the intertidal-supratidal cycle and the subtidal-supratidal cycle. According to the characteristics of sedimentology and the analysis of the Fischer Plot, the cycles are formed in the upland systern domain of the 3rd order sequence and controlled by Milankovitch-induced high-frequency sea-level fluctuation. The dolomitic limestone reservoirs...

Two kinds of meter-scale carbonate cycles are developed in the Bioclastic Limectone Member of the Bachu Formation in the Lower Carboniferous of the Tarim Basin, i. e. the intertidal-supratidal cycle and the subtidal-supratidal cycle. According to the characteristics of sedimentology and the analysis of the Fischer Plot, the cycles are formed in the upland systern domain of the 3rd order sequence and controlled by Milankovitch-induced high-frequency sea-level fluctuation. The dolomitic limestone reservoirs developed with neediehole-like solution openings may be related to the short-term exposure of carbonate platforms caused by the high-frequency sea-level fluctuation.

塔里木盆地下石炭统巴楚组生屑灰岩段发育两类米级碳酸盐旋回,即潮间-潮上旋回和潮下-潮上旋回。根据沉积学特征及Fischer图解分析,这些米级旋回形成在三级层序的高位体系域,受米兰柯维奇轨道参数诱导的高频海平面变化所控制。发育针孔状溶孔的云灰岩储层与高频海平面变化所引起的碳酸盐台地的短期暴露有关。

 
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