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magma相关的网络例句

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与 magma 相关的网络例句 [注:此内容来源于网络,仅供参考]

Lava from the earth's crust deep place, because the earth's crust deep place's temperature is extremely high, the lava by the volcano rock magma's shape existence, along with the volcanic eruption, the rock magma also spouts the surface along with it, meets the water or the low temperature starts to congeal, because the congealment process air entry, turned solid the rock magma to form the massive air bubbles gradually in the interior, coagulated after completely, has formed the structure unique lava.

火山石来自地壳深处,由于地壳深处的温度极高,火山石以火山岩浆的形态存在,随着火山喷发,岩浆也随之喷出地表,遇到水或低温开始凝结,凝结的过程由于空气的进入,逐渐变成固体的岩浆在内部形成了大量的气泡,完全凝固后就形成了构造独特的火山石。

The magma ofⅠ-⑥Concealed orebody experienced three stages:first,the deep liquation and pulsatory injection of the Cu- and PGE-rich magma; second,the concentration of tectonic activation;third,the later magma hydrothermal superposition.

探讨了来源于地幔深部的高镁玄武岩浆,在深部岩浆房和阶段岩浆房熔离分异时,富矿岩浆和矿浆之间存在富矿岩浆。

Gravitative differentiation occurred to the magma in the magma chamber, resulting in the increasing of basicity in the upper intrusive lithofacies and the better ore potential, and subsequently copper and nickel sulphides were formed by the ore magma injection.

熔浆在岩浆房发生了重力分异作用,致使其上侵岩相基性程度逐渐增高,含矿性也越来越好,最后由矿浆贯入形成了铜镍硫化物矿体。

The magma mingling between mafic magma and felsic magma is the primary mechanism responsible for the granitoids of crust-mantle mixed source.

镁铁质岩浆与长英质岩浆之间的混合作用是导致壳幔混源花岗岩类形成的主要机制。

The late bearing-ore magma formed by the differentiation and immiseibility of magma may form the intrusive iron body, but more iron deposits attribute to skarn type resulted from the metasomatic reaction between intrusive magma and stratum.

岩浆分异或不混溶作用形成的晚期含矿岩浆可以形成矿浆贯入型铁矿,更多的是侵入岩浆与地层发生交代反应形成的矽卡岩型铁矿。

The comparison of petrology, lithofacies, petro-geochemistry and tectonic environment of the rapakivi granite both from Qinling-Kunlun and world shows that the rapakivi granite has same or consistent characteristics: rapakivi structure, sub-aluminous, high-potassic, alkali-rich magma, two-peak magma assemblage and formed in post-collision environment. However, there are some certain differences in some geochemical index, forming age of magma, and geotectonic position of outcropping.

通过秦岭-昆仑造山带中的环斑花岗岩同世界元古宙环斑花岗岩的岩石学、岩相学、岩石地球化学和构造环境等方面的对比研究发现,二者具有相同或一致的特征:具环斑结构,属准铝、高钾、富碱岩浆,具双峰式岩浆组合,形成于后碰撞环境,但其地球化学的某些指标、岩浆形成时代和出露的大地构造位置等有一定差异。

The main clues of the study are the emplacing stage of Jinchuan ultrabasic magma and the evolutional model of magma.Its main research contents are the metallogenic epoch,the ore-forming mechanism,the emplacement mechanism,the magma evolutional-metallogenic model of Jinchuan Cu-Ni sulfide Deposit,the geological characteristics and genesis ofⅠ-⑥Concealed Cu-rich orebody.Its purpose are to predict the prospecting target area in the depth and border of Jinchuan Deposit and serve the Jinchuan mine.

本文以金川超基性岩浆侵位期次、岩浆演化模式为研究主线索,以金川铜镍硫化物矿床的成矿时代、成矿作用机制、就位机制、岩浆演化—成矿模型、Ⅰ-⑥富铜隐伏矿体地质特征及成因研究为重点内容,以预测矿区深边部找矿靶区服务矿山生产为目的。

Under the action of the active faults stretched deeply to magma chambers,the mantle gas released directly from the magma chambers by taking the faults as the paths is characterized by the CO2/3He ratios of 107~109 which are lower than the ones of the original mantle gas just separated from basalt magma.

我国五大莲池、云南腾冲、吉林长白等火山活动区温泉释放的幔源气体CO2/3He比率受到幔源气体释放机制的控制,在深切岩浆房的断裂活动作用下,以断裂为通道直接自岩浆房中释放的幔源气体,以低于幔源气体脱离岩浆时的CO2/3He比率为特征,其比率为 107~109。

Under the action of the active faults stretched deeply to magma chambers,the mantle gas released directly from the magma chambers by taking the faults as the paths is characterized by the CO2/3He ratios of 107~109 which are lower than the ones of the original mantle gas just separated from basalt magma.

摘 要 我国五大莲池、云南腾冲、吉林长白等火山活动区温泉释放的幔源气体CO2/3He比率受到幔源气体释放机制的控制,在深切岩浆房的断裂活动作用下,以断裂为通道直接自岩浆房中释放的幔源气体,以低于幔源气体脱离岩浆时的CO2/3He比率为特征,其比率为 107~109。

The location of rockbody and orebody is controlled by the activity center of ore-bearing magma and ore pulp,among which the most critical controlling factor is the magma conduits connecting with the activity center of ore-bearing magma and ore pulp.

4岩体的定位受含矿岩浆、矿液活动中心的控制,而最关键的控制因素还是与岩浆、矿液活动中心相连接的岩浆通道的出口。

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