Mobile
Log In Sign Up
Home > chinese-english > "结晶基底" in English

English translation for "结晶基底"

crystalline basement

Related Translations:
尿酸结晶:  uric acid crystal
结晶氧化铝:  crystal alumina
结晶习惯:  crystal habit
结晶习性:  crystal habit
结晶冰糖:  crystal candy sugar
结晶剂:  crystallizing agent
结晶橡胶:  crystalline rubber
结晶化学分析:  crystal chemistry analysiscrystalchemistryanalysiscrystallochemical analysis
结晶键:  crystal bridge
结晶熔化:  watery fusion
Example Sentences:
1.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。
2.Stratum composition in xiaoqinling represents early precambrian crystal basement and mesoproterozoic era cover rocks of the typical north china craton
小秦岭区内地层具有典型华北型早前寒武结晶基底和中元古代以来的盖层结构,不发育晚古生代、中生代构造层。
3.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。
4.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。
5.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。
6.During the yanshanian phrase , the area is in the condition of contractional background , with multi - staged tectonic reversion . 5 . through studying the origin of volcanic rocks and the characteristics of magma evolution , it concludes that there exist 3 originated areas of magma - from mantle , crust , and mantle - crust exchange . the basic magma of nandaling volcanic rocks of early jurassic is derived from upper mantle ; the magma of tiaojishan volcanic rocks of mid jurassic is formed in the contractional tectonic setting , and derived from the transition zone of crust and mantle interaction ; the acid magma of l
5 、通过岩石化学、微量元素、稀土元素的研究,探讨了不同级别节律的火山岩成因、岩浆演化等特征,认为本区燕山期火山岩有三个岩浆源区,即地幔源、地壳源和壳幔混源,早侏罗世的南大岭旋回的基性岩浆,起源于上地幔;中侏罗世髫髻山旋回火山岩是在相对挤压环境中,岩浆起源于壳幔过渡带;晚侏罗世无负eu异常的酸性岩浆来源于下地壳的古老结晶基底的局部熔融,有负eu异常的酸性岩浆来源于上地壳的局部熔融;早白垩世火山岩基性岩浆起源于上地幔,中性岩浆起源于下地壳底部的壳幔过渡带。
7.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。
8.The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement , while the cover has undergone the evolution of intra - continental rife in permian , down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary . the main sediments are huge - thick volcanic rock , shallow intrusive rock and tuff in early permian , dark mudstone , marl and muddy dolostone in lucaogou formation in middle permian , huge thick volcanic rock , intruder in tiaohu formation in middle permian , miscellaneous sandy gravel , sandstone and gray mudstone in triassic ( the red is under the gray , and huge - thick dark gray , gray sandy gravel , sandstone , mudstone with coal layer in jurassic
盆地基底由前寒武纪结晶基底和古生代褶皱基底组成,盆地盖层则经历了二叠纪的裂谷盆地、三叠纪?白垩纪的坳陷盆地和第三纪后的山间盆地的演化过程。盆地主要沉积了下二叠统巨厚火山岩、浅成侵入岩和凝灰岩;中二叠统芦草沟组的暗色泥岩、泥灰岩、白云质岩石以及条湖组的巨厚层火山岩、侵入岩;三叠系杂色砂砾岩、砂岩及灰色泥岩(下红上灰) ;以及侏罗纪厚层深灰、灰色砂砾岩、砂岩、泥岩夹煤层。
9.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。
10.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。
Similar Words:
"结晶化学元素" English translation, "结晶磺胺" English translation, "结晶灰岩" English translation, "结晶浑浊" English translation, "结晶或熔化热" English translation, "结晶机" English translation, "结晶机理" English translation, "结晶机制" English translation, "结晶极限" English translation, "结晶级聚对苯二甲酸乙二酯" English translation