Continental crust
- 网络大陆地壳
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Changing relation between tectonic gradations and continental crust dynamic mechanisms
构造层次与大陆壳动力学机制转变关系
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A huge thermal dome structure was firstly formed in continental crust due to rising of hot mantle plume during the Early Permian , and graben and fault basin were further formed .
早二叠世时,由于热地幔柱上升活动,引起在大陆壳区首先形成巨大的热穹窿构造,再进一步发展演化,形成地堑和断陷盆地。
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The most ancient parts of the continental crust are 4000 million years old .
大陆地壳最古老的部分有40亿年历史。
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Electrical property experimental studies on the mid and lower continental crust
大陆中、下地壳电学特征实验研究
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Review on recent research of the lower continental crust
大陆下地壳研究进展评述
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International Studies of the third tectonic element of continental crust
国际上对大陆地壳第三构造单元的研究
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Petrological model for structure of continental crust in East Hebei Province
冀东陆壳结构的岩石学模型
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Chemical compositions of continental crust and rocks in eastern China
中国东部地壳元素丰度与岩石平均化学组成研究
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Evolution of the continental crust is closely related to partial melting .
地壳分异演化与熔融作用密切相关。
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The Chemical Composition of the Continental Crust in Xinjiang Region , Northwestern China
新疆地壳的化学成分
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The Possible Effect of Hydrogen on the High Electrical Conductivity in the Lower Continental Crust
大陆下地壳高电导率的起源:矿物中的结构水
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International Symposium on Deep Structure of The Continental Crust
大陆地壳深部构造国际学术讨论会
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Review of the mechanism of the high conduction layers in middle to lower continental crust
中下地壳高导层成因研究综述
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Continental Crust is the inevitable product of formation and evolution of the Earth .
大陆地壳是地球形成演化的必然产物。
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The Nature of the Early Precambrian Continental Crust and Its Tectonic Evolution Model
早前寒武纪大陆地壳的性质与构造演化问题
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Chinese Continental Crust is One with Abundant Hydrocarbons
中国陆壳是富烃陆壳
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Laminar flow in the lower continental crust and its significance for continental dynamics
大陆下地壳层流作用及其大陆动力学意义
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Early Precambrian continental crust basement and its compositional features in South China
华南早前寒武纪陆壳基底及其组成特征
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Continental crust ( 2 ) C shape ; ( 3 ) D shape .
大陆地壳(二)
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Therefore , Chinese continental crust as a hydrocarbon-enriched one should be reasonable .
所以中国陆壳理应为富烃陆壳。
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The contents and distribution of carbon , sulphur and phosphorus in the continental crust of China
中国大陆岩石圈层碳硫磷的库存量及分配
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Average chemical composition of loess in china : as a good representative of the upper continental crust
中国黄土的平均化学成分:上部大陆地壳的一种典型代表
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Secondly , China continental crust has not only trisection structure but also dichotomy structure .
中国陆壳既有三分结构也存在二分结构;
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The Lower Continental Crust Composition Based on Discriminant Analysis of Global Granulite Terranes
全球麻粒岩相地体与大陆下地壳成分模型
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Seismic Reflection Response of Folds and Implications for Structural Geology of Continental Crust
褶皱的地震波反射响应及其大陆地壳构造地质意义
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Evidence for the presence of Early Paleozoic continental crust in Junggar Basin
准噶尔盆地早古生代陆壳存在的证据
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The geological-geochemical method in the study of the deep structure of continental crust and its application in South China
陆壳深部结构研究的地质地球化学方法及其在华南地区的应用
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Also Pb / Ce ratio is higher than island arc basalt and continental crust .
蛇纹石化橄榄岩的Pb/Ce比值远高于岛弧玄武岩和大陆地壳。
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Abundance of chemical elements in Oceanic and continental crust
大洋地壳和大陆地壳的元素丰度
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The continental crust is much thicker than average beneath the great mountain belts .
在高山地带下面的大陆地壳,其厚度要比平均厚度大得多。