結晶基底的英文

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英文翻譯
造句

crystalline basement

結晶 crystallize
基 base; foundation
底 bottom; base
拉張減薄的大陸結晶基底區 zone of stretched and thinned continental crystalline basement
基底結晶建造 fundamental crystalline formations
基底結晶建造；結晶地盾 fundamental crystalline formations
基底 basalia; base course; base of foundation; basement rock; basement-cover relationship; basis; bm; body; floor; foundation base; foundation bed; fundamental complex; fundus; ground; infrastructrue; infrastructure; planting; radical; radix; su trate; subbottom; subbase; substrate; substratum
單晶基板 monocrystal substrate; single crystal substrate
隱晶基斑狀 aphaniphyric
隱晶基斑狀；非顯晶基斑狀 felsiphyric
二期微晶基質 biphyletic mass
非顯晶基斑狀 aphanophyric
隱晶基斑狀的 aphanipyric
結晶 1.(析出晶體) crystallize2.(晶體) crystal 鹽結晶 salt crystals3.(成果) crystallization; fruit; product; quintessence; kristallization; valuable results; vegetate 勞動的結晶 the fruit of labor; 知識的結晶 quintessence of knowledge; 智慧的結晶 a crystallization of wisdom; 結晶玻璃 glass ceramics; 結晶槽 crystallization tank; 結晶層 crystallizing layer; 結晶度 crystallinity; degree of crystallization; 結晶斷面 [化學] crystalline fracture; 結晶固體 [化學] crystalline solid; 結晶核 nuclei of crystallization; nucleus of crystallization; 結晶化學 crystal chemistry; 結晶基底 crystalline basement; 結晶劑 crystallizing agent; 結晶結構 crystal structure; 結晶凈化 purging by crystallization; 結晶器件 crystallizer; 結晶盤 crystallizer pan; 結晶器 crystallizer; 結晶水 water of crystallization; crystal water; 結晶速度 crystallization rate; crystallization velocity; crystalline growth velocity; 結晶體 acicula; aciculas; 結晶溫度 crystallization temperature; 結晶學 crystallography; 結晶巖石 crystalline rock; 結晶窯 crystallization kilns; 結晶釉 crystal glaze; 結晶作用 crystallization
基底板, 基底層 laminae basalis
底, 基底 basi-
底,基底 fundi
底版，基底 b base plate; bbase plate
峰基底 peak base
負基底 negative base
古基底 palaeobasement; palaeosole
基本；基底 base
基底；基座 main bottom
基底板 lamina basialis
基底布 primary backing fabric

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例句與用法

The middle proterozoic granitoids was an intraplate type producted in transitinal crystalline basement before plate collision
中元古界的花崗巖類是板塊碰撞前過渡性結晶基底上局部熔融花崗巖類。
Stratum composition in xiaoqinling represents early precambrian crystal basement and mesoproterozoic era cover rocks of the typical north china craton
小秦嶺區內地層具有典型華北型早前寒武結晶基底和中元古代以來的蓋層結構，不發育晚古生代、中生代構造層。
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亞板塊南緣，具有前寒武紀結晶基底和古生代火山巖-碎屑巖褶皺基底組成的雙重基底。
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
研究認為，結晶基底在拼貼焊合過程中，其地體拼貼面之間焊合程度較差的界面在后期各階段的構造活動中，與上覆地層發生禍動。
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
它們與蘇格蘭阿帕拉契亞的加里東事件完全不同，在中國大陸出現了西域板塊完成拼合，華夏板塊構成統結晶基底，南揚子板塊廣泛發育板內褶皺，此時還形成了阿爾泰額爾古納碰撞帶等重要構造事件，而以中朝和北揚子板塊為代表的其他板塊則主要表現為穩定沉積，地塊運移，并呈離散狀態。
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 、通過巖石化學、微量元素、稀土元素的研究，探討了不同級別節律的火山巖成因、巖漿演化等特征，認為本區燕山期火山巖有三個巖漿源區，即地幔源、地殼源和殼幔混源，早侏羅世的南大嶺旋回的基性巖漿，起源于上地幔；中侏羅世髫髻山旋回火山巖是在相對擠壓環境中，巖漿起源于殼幔過渡帶；晚侏羅世無負eu異常的酸性巖漿來源于下地殼的古老結晶基底的局部熔融，有負eu異常的酸性巖漿來源于上地殼的局部熔融；早白堊世火山巖基性巖漿起源于上地幔，中性巖漿起源于下地殼底部的殼幔過渡帶。
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
對比研究表明，雖然它們各具特色，就脈型富大鈾礦床成礦作用而言，它們又具有較多的共性：重要成礦區的火山噴發皆奠基在古老的結晶基底上；古裂谷（或裂陷）既控制了火山巖帶的發育，又是有利的成礦構造背景；鈾礦賦存對火山巖的巖性沒有明顯的選擇性；鈾成礦的深部控制作用明顯；聯通的構造網絡系統是形成富大鈾礦的必要條件。
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
盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白云質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖(下紅上灰) ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。
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區域地質資料和最新的地層、巖系劃分對比資料，對鄂爾多斯盆地結晶基底的巖系分布、形成、演化以及斷裂的展布特征進行了描繪，并指出盆地基底與tg反射層之間的g層是薊縣系官道口群向盆地的延伸，盆地中原劃分的長城系、薊縣系地層可以和賀蘭山出露的黃旗口組、王全口組對比，亦劃歸青白口系，從而否定了鄂爾多斯盆地存在滹沱期坳拉谷和盆地中有中元古坳拉谷發育階段的看法。
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
論文以板塊構造研究的最新地體拼貼理論為指導，以巖系、地層為基礎，將沉積與構造分析相結合，并以地層學、巖石學、沉積學、構造地質學、遙感地質學、地球物理學、大地構造學等多學科入手，在充分整理現有資料及前人研究的成果基礎上，利用盆地周緣野外露頭以及盆地中部分鉆井深部取芯資料、地球化學分析資料、地震、非地震等資料將鄂爾多斯盆地置于一個更大的尺度，更深的范疇，討論了鄂爾多斯盆地及其周緣地區結晶基底與淺層構造之間的關系，探討了深部地質對盆地蓋層的影響，以不與前人雷同的視角對鄂爾多斯盆地基底發育及其蓋層中存在的問題提出了新的觀點和認識。