1)Sedimentary basin沉积盆地
1.Analysis of the key control factors of the formation of lithological stratigraphic traps in sedimentary basins;沉积盆地岩性地层圈闭成藏主控因素分析
2.Prospectivity for oil and gas in sedimentary basins superposed on arc-like folded belts in Mongolia;蒙古弧形褶皱带上叠沉积盆地油气远景
3.Genetic mechanism of non-hydrocarbon gas in China sedimentary basin;中国沉积盆地非烃气成因机制研究
英文短句/例句
1.Types and Main Characteristics of Devonian Sedimentary Basin in South China华南泥盆纪沉积盆地类型和主要特征
2.The sedimentary basin of Devonian in Southern Guizhou, South China is euxinic.黔南泥盆纪沉积盆地是一个停滞缺氧盆地。
3.TYPES OF LATE PALEOZOIC SEDIMENTARY BASINS AND THEIR SEDIMENTARY CHARACTERISTICS IN NORTHERN XINJIANG新疆北部晚古生代沉积盆地类型及其沉积特征
4.Sequence and Depositional Architecture of Sedimentary Basin and Process Responses沉积盆地的层序和沉积充填结构及过程响应
5.Devonian Sedimentary Basins in Hunan: Evolution and Sequence Stratigraphic Model湖南泥盆纪沉积盆地的演化与层序地层沉积模式
6.DEVONIAN SEDIMENTARY ENVIRONMENTS AND BASIN EVOLUTION IN ZHASHUI-ZHENAN DISTRICT, EASTEPN QINLINC CHIAN东秦岭柞水—镇安地区泥盆纪沉积环境和沉积盆地演化
7.Later Triassic-Middle Jurassic Basin History of Qiangtang, Northern Tibet, China;羌塘盆地晚三叠世—中侏罗世早期沉积盆地演化
8.hydrogeology of great sedimentary basins大型沉积盆地水文地质学
9.Relationship between Groundwater and Hydrocarbon Accumulation-Preservation in Sedimentary Basin沉积盆地地下水与油气成藏-保存关系
10.GEOLOGICAL FEATURES OF DEVONIAN SEDIMENTARY BASINS IN SOUTH CHINA AND THEIR DEPOSITION AND MINERALIZATION华南泥盆纪的沉积盆地特征沉积作用和成矿作用
11.FORMING MECHANISM OF THE DEVONIAN VOLCANO-SEDIMENTARY BASIN OF THE SOUTHERN ALTAY MARGIN阿尔泰南缘泥盆纪火山－沉积盆地形成机制探讨
12.Basin Evolution and Distribution of Lacustrine Systems in Middle and Upper Eocene,Dongying Basin东营盆地始新统沉积体系及盆地演化
13.Jurassic sedimentary system and basin evolution in tidal basin潮水盆地侏罗系沉积体系及盆地演化
14.Sediment Character and Sediment Environment of the Cretaceous Period Stratum in Lasa Basin拉萨盆地白垩纪地层的沉积特征及沉积环境
15.SEDIMENTOLOGY AND SEDIMENTARY EVOLUTION OF LOWER CRETACEOUS LAIYANG FORMATION IN JIAOLAI BASIN胶莱盆地下白垩统莱阳组沉积作用和沉积演化
16.Tectonic Euolution and Sedimentation of JianChan Mesagaic Basin in Western Liaoning Province;辽西建昌盆地中生代的构造演化与盆地沉积
17.Sedimentary Evolution of Paleogene Series in Deep Water Area of Zhujiangkou and Qiongdongnan Basin珠江口盆地—琼东南盆地深水区古近系沉积演化
18.PERMIAN SEDIMENTARY FACIES AND PALAEOGEOGRAPHY IN ILl BASIN伊犁盆地二叠纪沉积相及古地理特征
相关短句/例句
sedimentary basins沉积盆地
1.Tectono-thermal modeling of sedimentary basins:review and outlook;沉积盆地构造热演化研究进展:回顾与展望
2.With introduction and discussion of the dynamics of sedimentary basins and basin reservoir(ore) forming systems to be a main line,this paper generalizes and summarizes author's thoughts and viewpoints in this area.以沉积盆地动力学与盆地成藏(矿)系统为主线,梳理和归纳了笔者在此方面理论研究的部分认识和观点。
3.As an important means of geofluids research,the fluid inclusion study has played an significant role in the study on the formation environment of petroleum reservoir,the relationship among the coexisted organic & inorganic mineral deposits in sedimentary basins.流体包裹体作为地质流体研究的重要手段,在沉积盆地油气成藏条件分析和有机/无机矿产共存、共生关系研究中起着不可替代的作用。
3)basins sedimentation盆地沉积
4)basin sediments盆地沉积物
5)sedimentary basin tract沉积盆地域
1.On the basis of analysis for the character of stratigraphic interface and the depositional architecture of genetic stratigraphic units, the stratigraphic sequence of Permian to Trassic is divided into seven depositional episodes, three tectono-depositional episodes and two sedimentary basin tracts, and the evolutional cours.在分析地层界面性质和各类成因地层单位沉积构成的基础上,将华南二叠-三叠系划分为7个沉积幕、3个构造沉积幕和2个沉积盆地域,恢复了华南板块二叠-三叠纪的演化过程,论述了板块构造运动、海平面升降和源区侵蚀作用对各级成因地层单位的控制意义,证明了华南的古特提斯海经历了陆表海和伸展裂谷海两个演化阶段。
6)depositional basinal water沉积盆地水
延伸阅读
阿克赛钦盆地 半封闭性山间盆地。位于和田南部昆仑山与喀喇昆仑山间，地质构造上北为西昆仑山背斜带，南为古生代褶皱带。东南部的地表径流归宿于山间局部洼地，形成许多咸水湖，如阿克赛钦、萨利吉勒及腾格湖，属封闭性部分。西北部地表径流汇集为喀拉喀什河，流至塔里木盆地，为和田河西源，属外泄性山间盆地性质。盆地海拔几乎都超过4000米，而位于喀拉喀什河谷的康西瓦，为3986米;东南部的阿克赛钦湖,湖面海拔为4990米；萨利吉勒湖，湖面为5181米。盆地内的山峰大多超过6000米,山口大多超过5000米。如喀喇昆仑山口为5568米,其东南的天文点为5565米;空喀山口5278米。因海拔高,全属高寒气候。 以康西瓦为例，年均温-0.6℃，1月均温-11.3℃，7月9.8℃，无霜期10天,10℃以上活动积温仅20℃。天文点年均温-9.8℃，1月均温-21.0℃，7月3℃。盆地位于雨影面,西南季风很难越过喜马拉雅山进入,西风气流也难越过喀喇昆仑山和西昆仑山，实测年降水量均不到100毫米，康西瓦36毫米，天文点47毫米,空喀山口仅29毫米。盆地虽然地处高寒,但地势较平坦,且有几处山口可至克什米尔地区，自古以来为新疆至印度次大陆以及从塔里木盆地经克什米尔至中东各国的捷径。南疆各地去沙特阿拉伯朝圣的穆斯林，过去多取此道。中华人民共和国成立后,建成新疆至西藏阿里地区公路,通过阿克赛钦盆地的线路约400公里,至喀喇昆仑山口、空喀山口等边防点也有公路。盆地矿产资源丰富，北部已作初步查勘,从康西瓦至大红柳滩间为伟晶岩密集区,已发现电气性能良好的工业云母，伴生锂、 铍、铌、 钽、铷等稀有金属。并发现近20条锂辉石矿脉，大多可露天开采。
