克拉通

基本解释 (translations)

craton

与克拉通相关的网络例句 [注：此内容来源于网络，仅供参考]

The P-wave velocity-depth profile and electrical conductivity-depth profile can be calculated from the experimental data and the fundamental geothermal parameters in northern margin of the North China craton. The comparison of the calculated results with the elastic and electrical structure of this area reveals that the v of amphibolite is approximately equal to the middle crust, the electrical conductivity of amphibolite intersects the range of the middle and lower crust in this area.

利用实验获得的弹性波纵波速度及其温度系数和压力系数以及电导率与温度的关系，结合现今华北克拉通地热学的基本参数，计算得到斜长角闪岩的弹性波纵波速度－深度剖面和电导率-深度剖面，将二者分别与华北克拉通北缘深部地壳的弹性及电性结构进行对比的结果表明：高温高压下绿泥石化斜长角闪岩的弹性波纵波速度与该地区中地壳速度相当，电导率介于中、下地壳范围内。

There have developed four types of caprock , namely Kraton or transitional facies caprock , limnetic facies coal measure caprock , oxidation basin valley or adjacent marine facies cream mudstone caprock ,and lacustrine mudstone caprock .

中西部前陆盆地沉积演化经历前前陆盆地克拉通沉积、早期前陆盆地沉积、中生代坳陷盆地沉积和新生代再生前陆盆地沉积四个阶段，共发育四种类型的盖层：即克拉通或海陆过渡期盖层、湖沼相煤系盖层、氧化宽浅湖或边缘海相膏泥岩盖层和湖相泥岩盖层。

Molybdenum deposits generally occur in nearly E-W direction along the tectonic lineament and are mostly concentrated in a zone stretching from Jinduicheng area of Shaanxi Province in the west to Nannihu-Sandaozhuang-Shangganggou area of Luanchuan and Leimenggou of Songxian in western Hena...

研究结果表明：除黄龙铺钼矿床形成于(221.5±0.3)Ma外，东秦岭地区钼矿床的大规模成矿主要出现在(144.8±2.1)~(132.4±2.0)Ma时限之间，对应的地球动力学背景为华北克拉通与扬子克拉通的碰撞造山后陆内造山局部伸展过程、中国东部地球动力学体制大转换晚期岩石圈拆沉及伸展时期。

Magmatic intrusion and its related surfacial deformation in the margin of Craton are the superficial response and representation of the inter action between crust and mantle, as well as one of the records of development from reactivated Craton to orogenesis process.

中文摘要：克拉通边缘岩浆侵位及其相关的浅层构造变形制约，不仅是深部壳幔相互作用及区域构造应力作用的浅部响应和表现，而且是从克拉通活化发展到造山作用的物质和事件记录之一。

All these evidences suggest that the present outcropping basements of the Yangtze craton are free of a united evolutionary history.

与已有数据相结合，初步认为扬子克拉通目前所出露的基底没有统一演化历史，对扬子克拉通的基底有待更深入的研究。

The Huade Group underwent at least two phases of deformation:the early phase of deformation gave rise to ENE-trending synclinorium and the late phase was marked by tectonic superimposition,forming NNW-trending folds. The main phase of deformation likely occurred in ~2.0 Ga B.P.The deformation of the Huade Group is related to a Paleoproterozoic orogenic event along the northern margin of the North China Craton, which has great significance for the study of accretion and breakup of the North China Craton.

化德群经历了两期构造变形，早期为北东东走向的复式向斜，晚期又遭受了构造叠加，形成了北北西向褶皱构造，其主期变形可能发生在2.0 Ga左右，它的褶皱造山是华北克拉通在古元古代向北增生的体现，这对研究华北克拉通的增生，裂解具有重要意义。

Pulling setting presents in southern China in Permian forming rift basins, which extends and develops from the edge to the inside of continent. Under the influence of Dongwu movement, two second order cycles forming by up and down of sea level happened in Yangtze and Huaxia craton. Rift basins in continental margin are primary sedimentary location of LST. But craton areas are the main deposition area of TST and HST. Weathering on land and river sediment or only thin coaly clasolite of marsh facies present mainly in LST deposition.

二叠纪我国南方总体处于拉张背景，发育了由陆缘向陆内延伸发展的裂陷盆地；受东吴运动影响，扬子和华夏克拉通遭形成了两个二级海平面升降沉积旋回；陆缘裂陷盆地是低位期沉积的主要场所，而克拉通区主要为海侵和高位期沉积，低位期主要表现为陆上风化残积、河流沉积或仅发育厚度很薄的沼泽相含煤碎屑岩。

Based on the petroleum system division of our predecessors, the petroleum systems of Chinese marine basin s can be divided into six types, that is, the aulacogen and its succeeding syneclise, the craton basin, the craton peripheral subsidence basin, the foreland basin, the strike slip basin and the epicontinental fault basin petroleum system.

该文在总结前人油气系统分类的基础上，将中国海相盆地油气系统划分为 6种类型，分别为坳拉槽及其后期的台向斜油气系统、克拉通盆地油气系统、克拉通周边沉降盆地油气系统、前陆盆地油气系统、走滑盆地油气系统和陆缘裂陷盆地油气系统。

We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

在综述前人认识的基础上，笔者通过对中国前陆盆地的构造演化历程、沉积充填特征、构造成因及其空间分布规律、构造变形特征等的研究，提出了中国前陆盆地构造地质发育的5个主要特征：(1)两种不同性质的原型盆地发生正反转的叠合性，即挤压构造下作为&本体&的前陆层序与拉张构造下作为&基础&的裂谷、断陷盆地之间的叠置；(2)显生宙以来中国大陆先后发生了4期前陆冲断构造演化的多期性，它们分别是加里东晚期、海西晚期、印支期和喜马拉雅晚期；(3)基于小克拉通基底拼贴后在造山带前缘复活再生的继承性，即统一拼合大陆内部的构造变形导致古造山带的复活，在古造山带边缘发育新生代前陆盆地或前陆冲断带；(4)在空间分布上受环青藏高原巨型盆山体系控制发生陆内变形的系统性，在环青藏高原巨型盆山体系内构造变形强度、盆地沉降幅度、盆山耦合程度等从内环向外环依次降低，从古造山带向克拉通方向构造变形强度依次降低，构造变形样式逐渐简单、构造变形时间依次变新；(5)前陆冲断带的构造样式由于受边界力学条件和沉积地层介质作用而具有多变性，存在沉积盖层内脆性变形的断层相关褶皱、造山带前缘韧性变形的基底卷入构造、与走滑构造相伴生的基底卷入的断层相关褶皱、盆地内部塑性变形的盐构造。

It is suggested that North China and Yangtze Cratons had ever been a unified craton, called Palaeosinica Craton, within which NNE-trending structural framwork was dominant, untill to the end of Palaeoproterozoic.

提出了 古元古代华北克拉通与扬子克拉通可能为一个统一的克拉通，暂称之为古中国克拉通，并且这一克拉通内的主导性构造线方位是NNE向。

与克拉通相关的网络解释 [注：此内容来源于网络，仅供参考]

Archean craton：太古代克拉通

archean basement 弧形基底 | Archean craton 太古代克拉通 | Archean era 太古代

Archean craton：太古代克拉通,太古代古陆

"Archaias","原始虫属,古虫属(有孔虫类,E2-Q)" | "Archean craton","太古代克拉通,太古代古陆" | "archegonial chamber","藏卵室"

Clark University：克拉克大学

因为喜欢三十年代的诗人徐志摩,所以特意乘通勤火车从波士顿出发去西面的Worcester克拉克大学(Clark University)游览,据说,徐志摩就是在那里获得了荣誉学士.

cratonic embayment：克拉通支地槽

cratonic crust 克拉通地壳 | cratonic embayment 克拉通支地槽 | cratonic margin 克拉通边缘

kratogenic：克拉通的

kratogenic area 克拉通区 | kratogenic 克拉通的 | kraton 克拉通

kratogenic area：克拉通区

kratochvilite 芴石 | kratogenic area 克拉通区 | kratogenic 克拉通的

rifted cratonic margin：裂谷化克拉通边缘

rifted arch basin ==> 拱顶断陷盆地 | rifted cratonic margin ==> 裂谷化克拉通边缘 | rifted margin prism ==> 裂谷边缘沉积柱

craton：克拉通

垂直运动速度缓慢、幅度小,沉积作用广泛而较均一,岩浆作用、构造运动和变质作用也都比较微弱. 地台区的外形呈近似圆形,直径可达数千千米,是地壳大地构造中相对稳定的构造单元. 在文献中有"克拉通"(Craton)一词,意义大致与此相当.

continental craton：大陆克拉通

continental convergence 大陆汇聚 | continental craton 大陆克拉通 | continental crust stem 大陆壳套

epeirocratic craton：陆地克拉通

epeirocratic condition 造陆优势期 | epeirocratic craton 陆地克拉通 | epeirocratic period 造陆期