crystalline basement中文是什么意思

• 结晶基底

• "crystalline"中文翻译    adj. 水晶的，由水晶做成的；结晶的，【化、矿】结晶质 ...
• "basement"中文翻译    n. 1.建筑物的底部。 2.【建筑】底层；地下室 〔c ...
• "basement" 中文翻译 :    n. 1.建筑物的底部。 2.【建筑】底层；地下室 〔cf. cellar〕.
• "crystalline" 中文翻译 :    adj. 水晶的，由水晶做成的；结晶的，【化、矿】结晶质的；透明的。 n. 结晶质，结晶体，晶态；(眼球)水晶体。
• "acoustic basement" 中文翻译 :    声波基底; 声学基底
• "american basement" 中文翻译 :    包括房屋主要人口的地面上的底层
• "arc basement" 中文翻译 :    岛弧基底
• "archean basement" 中文翻译 :    弧形基底
• "ash basement" 中文翻译 :    出灰间
• "bargain basement" 中文翻译 :    (地下室)廉价部。
• "bargain-basement" 中文翻译 :    adj. 便宜的，质量不佳的。
• "basement (l02)" 中文翻译 :    底层；地窖；基层
• "basement anisotropy" 中文翻译 :    基底非均质性
• "basement area" 中文翻译 :    地下掩蔽部
• "basement block" 中文翻译 :    基底断块
• "basement complex" 中文翻译 :    【地质学；地理学】基地杂岩。
• "basement concourse" 中文翻译 :    地下中央大厅
• "basement contour" 中文翻译 :    基底等深线
• "basement cullet" 中文翻译 :    炉底碎玻璃
• "basement door" 中文翻译 :    地下室门
• "basement drain" 中文翻译 :    地下室排水
• "basement drainage" 中文翻译 :    地下室排水
• "basement dwelling" 中文翻译 :    地下住宅
• "basement effect" 中文翻译 :    底层效应
• "basement entrance" 中文翻译 :    地下室入口

• On the age of metamorphic rocks of the yudongzi group and the archean crystalline basement of the qinling orogen
  鱼洞子群变质岩年龄及秦岭造山带太古宙基底
• The middle proterozoic granitoids was an intraplate type producted in transitinal crystalline basement before plate collision
  中元古界的花岗岩类是板块碰撞前过渡性结晶基底上局部熔融花岗岩类。
• Santanghu basin , located in the edge of the southern siberian plate , has the double basements of the pre - cambrian crystalline basement and the palezoic metamorphic basement of volcanic - sedimentary rocks
  三塘湖盆地位于西伯利亚板块南缘，具有前寒武纪结晶基底和古生代火山岩-碎屑岩褶皱基底组成的双重基底。
• And during each period of the process of the crystalline basement stick , the interface with relatively bad welding had coupled movement with the overlying layer . as a result , the overlying layer happen to be dip - slip drag
  研究认为，结晶基底在拼贴焊合过程中，其地体拼贴面之间焊合程度较差的界面在后期各阶段的构造活动中，与上覆地层发生祸动。
• Several important tectonic events took place in the chinese continent during the early paleozoic , such as the amalgamation of xiyu plate , forming a unified crystalline basement with the cathaysian plate , development of widespread intraplate deformations in southern yangtze plate , and the occurrence of altay - ergun collision zone
  它们与苏格兰阿帕拉契亚的加里东事件完全不同，在中国大陆出现了西域板块完成拼合，华夏板块构成统结晶基底，南扬子板块广泛发育板内褶皱，此时还形成了阿尔泰额尔古纳碰撞带等重要构造事件，而以中朝和北扬子板块为代表的其他板块则主要表现为稳定沉积，地块运移，并呈离散状态。
• The comparison study of the three belts indicates although they are distinct from each other all the three belts show many common features in the aspect of the metallogeny of large - rich vein uranium deposits , i . e : the important metallogenic areas are located above the old crystalline basement ; the paleo - rifting ( taphrogeny ) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment ; the occurrence of uranium deposit does not depend on the lithology of volcanic rocks ; uranium metallogeny is obviously constrained by deep geologic processes and the connected fault - structural net is the necessary condition for the formation of large - rich uranium deposits
  对比研究表明，虽然它们各具特色，就脉型富大铀矿床成矿作用而言，它们又具有较多的共性：重要成矿区的火山喷发皆奠基在古老的结晶基底上；古裂谷（或裂陷）既控制了火山岩带的发育，又是有利的成矿构造背景；铀矿赋存对火山岩的岩性没有明显的选择性；铀成矿的深部控制作用明显；联通的构造网络系统是形成富大铀矿的必要条件。
• A large amount of data of the latest regional geoglogy and the latest correlation data of layers and rock formation have been quoted , and a description of distribution of crystalline basement , formation , evolution as well as the distribution characteristic of the fracture belt of ordos basin have been made in this paper , and the paper also pointed out that the g - layer which lies between the base of the basin and tg reflector , is the extension of basinward of guandaokou of jixian system . the layer of changcheng system and jixian system , which had been divided before , can be correlated with the exposed huangqikou group and wangquankou group in helan mountain , and divided into qingbaikou system . so , the paper denied the viewpoint of the existence of aulacogen in hutuo period and middle proterozoic in this basin
  文中引用了大量最新的区域地质资料和最新的地层、岩系划分对比资料，对鄂尔多斯盆地结晶基底的岩系分布、形成、演化以及断裂的展布特征进行了描绘，并指出盆地基底与tg反射层之间的g层是蓟县系官道口群向盆地的延伸，盆地中原划分的长城系、蓟县系地层可以和贺兰山出露的黄旗口组、王全口组对比，亦划归青白口系，从而否定了鄂尔多斯盆地存在滹沱期坳拉谷和盆地中有中元古坳拉谷发育阶段的看法。
• It is directed by the 1atest theory of terrain stickin plate tectonic , and based o n petrographical series and stratum layers . from the aspects of structural analysis , stratigraphy , petrology , sedimentology , structure geology , remote sensing geology , geophysics as well as tectonics , the author put the ordos basin into a bigger and deeper studying field while using the combination of sedimentation and structure analyses , the data of outcrops around the basin and the deep drilling coring data in the middle of this basin , geochemistry analysis , seismic methods and non - seismic methods , etc . this paper discussed the relationship between the crystalline basement and the suprastructure in and surrounding the ordos basin , and also the influences of deep geology on the basin platform cover , and some new point of view and better understanding have been brought forward on the basement growth of ordos basin and it ' s platform cover
  论文以板块构造研究的最新地体拼贴理论为指导，以岩系、地层为基础，将沉积与构造分析相结合，并以地层学、岩石学、沉积学、构造地质学、遥感地质学、地球物理学、大地构造学等多学科入手，在充分整理现有资料及前人研究的成果基础上，利用盆地周缘野外露头以及盆地中部分钻井深部取芯资料、地球化学分析资料、地震、非地震等资料将鄂尔多斯盆地置于一个更大的尺度，更深的范畴，讨论了鄂尔多斯盆地及其周缘地区结晶基底与浅层构造之间的关系，探讨了深部地质对盆地盖层的影响，以不与前人雷同的视角对鄂尔多斯盆地基底发育及其盖层中存在的问题提出了新的观点和认识。