陆台

华北陆台侏罗－白垩纪岩石地层基本特征

Basic Development Characteristics of Jurassic Cretaceous Lithostratigraphy in North China Platform

华北陆台高压麻粒岩－榴闪岩韧性剪切带

The Ductile Searing Belts of High-Pressure Granulite-Garner-Amphibolite in North China Platform

华北陆台晚古生代岩相古地理

Lithofacies paleogeography of North China platform in Late Paleozoic

这枚自动制导火箭在受控下降后触及着陆台时发生爆炸。

The self-guided rocket as it on a landing pad following a controlled descent .

新疆天山北部山前拗陷带及准噶尔盆地陆台地质初步报告

A resume of geological data of North foreland of Tianshan and Dzungaria platform , Sinkiang

华北陆台北缘金矿类型及成矿区带

Gold metallogenic belts and zones in the North China platform and types of the gold deposits

西昆仑山北坡陆台盖层型元古宇的基本特征

Basic characteristics of Proterozoic EONOTHEM as a table cover on northern slope of Western Kunlun Mountain

华北陆台北缘基础地质问题与找矿前景

Some issues on basic geology and ore-search prospect on the north margin of North China Platform

华北陆台北缘晚元古代褶皱带变形&变质作用的显微构造研究

Microstructural Research on Deformation & Metamorphism of Late Proterozoic Fold Belt , North Margin of North China Platform

华北陆台上一个大型沉积盆地古生界油气的形成与演化

The formation and evolution of Paleozoic oil and gas in a large sedimentary basin in North China Platform

形成晶体的碳质来源不均一，反映了中元古代华北陆台下地壳岩浆成分的不均一性。

Heterogenity of the carbon source implies the magma beneath the North China platform was not homogeneous at Late Mesoproterozoic .

华北陆台北缘基底是由不同时代、不同特征的独立的构造单元组成的。

Basement of the North margin area of The North China platform includes separate tectonic units with different ages and characters .

专家们对华北陆台早前寒武纪基底构造格局形成与演化的认识既有共同点又有分歧。

There are two different ideas about the tectonic division of North China Block ( NCB ) basement and its evolution in early Precambrian .

根据华北陆台北缘金矿的赋存部位和富集特点，划分出9种金矿类型。

Based on location of gold deposits and Au enrichment characteristics Au deposits at the north margin of the north China platform are devided into 9 types .

内蒙古温都尔庙白乃庙地区是早古生代中亚蒙古海洋板块与华北陆台之间的海沟岛弧体系。

The wenduermiao Bailaimiao region in Inner Mongolia formed the trench island is a system between the central Asian Mongolia oceanic plate of Early palaeozoic and the North China continental platform .

华北陆台北缘金矿床的地球化学特征早前寒武纪花岗岩&绿岩地体中赋存着丰富的金矿床。我国绿岩带主要分布在华北陆台，也是重要的含金岩系。

GEOCHEMICAL CHARACTERISTICS OF GOLD DEPOSITS AT NORTH MARGIN OF THE NORTH CHINA CONTINENTAL TABLE , CHINA In the world a lot of gold deposits occur in the early Precambrian greenstone belts .

这五套含金建造中金含量较华北陆台区其它含金建造的金含量高，但是规模较小。

The gold contents in the five gold bearing formations are higher than those of other gold bearing formations in the North China Craton However , the scale of them are smaller .

相对于俄罗斯陆台沉积岩稀土平均值而言，水云母粘土和蒙脱石粘土全样中富集中，重稀土而轻稀土贫化，高岭石粘土则相反。

In comparision with the mean value of REE in Russian Table sediments , the damourite and askanite clay is rich in middle and high REE , but lack of light REE , kaolin is contrary .

花岗岩-绿岩地体内各岩石类型的岩石地球化学特征与国外太古宙及我国华北陆台花岗岩-绿岩带内同类岩石极为相似。

The lithogeochemical features of all types of rocks in the granite greenstone massif are very much similar to those of the same types in the Archean granite greenstone belts abroad and in North China platform .

山西辛庄金矿床位于华北克拉通中间带北部，山西陆台五台隆起西北侧与燕山沉降带西南缘两大构造单元相互嵌接的中生代构造岩浆活动带上，是中生代构造岩浆岩活化地区。

Xinzhuang gold deposit is located in the northern part of the North China Craton intermediate belt , and in a Mesozoic tectonic-magma activation area which is embedded by the two tectonic units-the northwestern Wutai uplifts of Shanxi platform and the southwestern Yanshanian subsidence belt .

开放陆资入台的前景由此变得渺茫起来。

That makes liberalising investment inflows a remote prospect .

结果表明：古老的陆核、原地台、地台和地块等稳定地区内部的密度值横向变化小，年轻的褶皱带等活动地区内部的密度值横向变化大。

The conclusion show that : the density horizontal change small inside the stable region of the old continental nucleus , original platform , platform , and massif but the density horizontal change big inside the movable region of young fold band .

大陆陆壳的形成与发展经历了陆核地块（台）联合大陆大陆裂解陆缘增生碰撞造山的演化过程。

The continental crust was formed through the continental nucleus , platform , Pangea , continental splitting , continental accretion , intercontinental collision and orogeny in its progress .