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geosynclinal相关的网络例句

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与 geosynclinal 相关的网络例句 [注:此内容来源于网络,仅供参考]

The geosynclinal tectonic layer was composed of sandstone-slate rocks of Lengjiaxi Group in the area.

湘东地区属于雪峰山构造带的东延部分,其区域地壳演化至少经历了前地槽、地槽、地台和地洼等构造发展阶段。

They are spatially res tricted by geosynclinal structural layer and are temporally controlled by Diwa stage.

本区金矿空间上受地槽构造层的制约,而成矿时代则受地洼阶段的限制,这就是本区金的成矿时代明显不同于世界其它地区的原因。

The evolution history of Victorian area can be divided into four stages which are pregeosynclinal stage, Geosynclinal stage, platform stage and Diwa stage. Each of them has some distinct characteristics.

它的演化历史可分为四个阶段,即前地槽阶段、地槽阶段、地台阶段和地洼阶段,每个阶段均具有明显的沉积建造、岩浆建造和构造型相等特征。

It is revealed that there exists the pre geosynclinal formation in the Xuefeng district .

研究表明,湖南雪峰地区存在前地槽构造层,该区金矿的成矿物质主要来自赋矿地层,成矿流体主要为大气降水,其主成矿期为加里东期、印支-燕山期。

The area of the geosynclinal structural layer in Diwa Region is favourable area for looking for greenstone belt type and metahydrothermal gold deposits.

在地洼区内有前地槽构造层或地槽构造层分布区寻找绿岩型金矿或变质热浓型金矿。

Researches to the gold-bearing quality of sedimentary and magmatic rocks show that most of these rocks have more gold content than the average of the upper crust. Further evidences are quoted to support the view that fluids exist in shallow crust have the ability resolve some gold. Moreover, in the convergent compression, deep melting of the lower lithosphere can bring some Au and mineralization materials and move up to upper crust. Regional faults, which formed in geosynclinal and diwa periods, controlled the partial distribution of intrusions and gold mineralization belts, i.e.

区域地层和岩浆岩的含金性表明,岩浆岩和大部分地层均具较高的金异常含量,而进一步的研究表明浅部地壳的流体对地层中的金具一定的溶解和搬运迁移能力;而在汇聚挤压构造体制下由深熔作用生成的岩浆可以从岩石圈深部携带部分金和其它成矿物质并迁移到地表浅部,地槽期和地洼期形成的区域断裂构造共同控制了中新世岩浆的侵入和金成矿带的分布。

Crustal movement ; geosynclinal closing ; Carboniferous ; N.

地壳运动;地槽封闭;石炭纪;新疆北部

West Sarawak, which located in the Northwest of Kalimantan island, geotectonically underwent geosynclinal, platform periods and now in diwa process. The geological and structural features of Lupar River regionhe west part of West Sarawak?

位于加里曼丹岛西北部的西砂捞越地区,大地构造经历了地槽、地台和地洼三个演化阶段,西砂捞越西部卢帕河地区的地质构造特征代表了自晚白垩世到渐新世期间北东洋壳对南西陆壳的汇聚挤压作用。

Tectonism in geosynclinal, platform and diwa stages, rifting, plate tectonics, magmatic intrusion, volcanic activity, hydrothermalism, metamorphism, hot deposition and related mineralization are manifestations of large-sdaled korizontal and vertical of HACONS fluids in the asthenosphere.

地壳中槽、台、裂谷、地洼、板块构造、岩浆侵入、火山、热液、变质、热沉积以及有关的成矿作用乃是软流层中幔汁大规模水平和垂直活动的种种表现方式。

The geotectonic evolution is divided into pre - geosynclinal phase, geosynclinal phaseO- T2X platform phase(T3 - J2 and Diwa phase (J3 - Q) in the Beishan area according to sedimentary formation and magatic formation.

根据沉积建造、岩浆建造将北山地区大地构造演化划分为前地槽阶段、地槽阶段(O-T_2)、地台阶段(T_3-J_2)和地洼阶段(J_3-Q),其中地槽阶段O—P_1属地槽期、P_2-T_2属褶皱造山期,D_(2-3)发生强烈的局部造山运动。

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从鲍尔点的形成原理出发,分析对称连杆曲线上鲍尔点的产生条件,提出等边机构的对称连杆曲线上有单鲍尔点和双鲍尔点。

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