说明:双击或选中下面任意单词,将显示该词的音标、读音、翻译等;选中中文或多个词,将显示翻译。
您的位置:首页 -> 词典 -> 基性岩浆侵入
1)  basic magmatic intrusion
基性岩浆侵入
2)  basic intrusive rock
基性侵入岩
1.
The initial rock of amphibolite in the Kuanping Terrane of West Henan Majukou areas in North Qinling is a basic intrusive rock(gabbro),and its isotime line age of whole rock Samarium(Sm)-Neodymium(Nd) isotope is 747.
北秦岭豫西马驹口地区宽坪岩群中的斜长角闪岩原岩为基性侵入岩( 辉长岩) ,其全岩的Sm-Nd 同位素等时线年龄为747-72±43Ma,钕同位素初始比值为εNd(t) = - 0。
3)  magma intrusion
岩浆侵入
1.
Influence of magma intrusion on reservoir features of surrounding mud rocks in rift basin-case study of gabbros in Chunxi area of Dongying Sag;
裂谷盆地岩浆侵入对泥质围岩储集性能的影响——以东营凹陷纯西地区辉长岩为例
2.
Preservation conditions of the coalbed methane in Tiefa mining area is systematically studied based on analyses of the lithology and sealing capability of the adjacent rocks of coal bed, later reformation, hydrogeologic conditions, and magma intrusion.
通过对铁法矿区煤层顶底板岩性及其封闭性能、后期改造、水文地质条件及岩浆侵入等几方面的分析,系统探讨了铁法矿区煤层气的保存条件。
3.
The influences of Magma intrusion activity on the clastic rocks include the magma upwarp activity, the baked activity and the hydrothermal activity.
基性岩浆侵入或喷溢活动中,岩浆中的Fe2+、Mg2+,有利于周围碎屑岩中的蒙脱石向绿泥石转化。
4)  magmatic intrusion
岩浆侵入
1.
Based on the statistics of exploratory boring data,the main characters are researched on magmatic intrusion in Qidong coalmine.
通过对祁东煤矿勘探钻孔统计资料分析,研究了岩浆侵入煤层的主要特征。
2.
Take the 3D seismic explore data as a basis, the ones that set up magmatic intrusion were theory models, on the basis of using the grey related analytical method in the grey systematic theory to carry on attribute to optimize, rely on BP network method in artificial neural network theory , has set up the BP network model that magmatic intrusion range and predicted.
以某矿三维地震勘探资料为依据,建立了岩浆侵入的正演模型,在应用灰色系统理论中的灰色关联分析方法进行属性优化的基础上,借助人工神经网络理论中的BP网络方法,建立了岩浆侵入范围预测的BP网络模型。
5)  intrusion of magma
岩浆侵入
6)  mafic magma intrusion
基性岩浆侵位
补充资料:超基性岩
超基性岩
ultrabasic rock 

    火成岩的一类。二氧化硅含量低(小于45%),铁、镁质含量高,以不含石英为特征。深灰黑色,比重较大。主要由橄榄石、辉石,以及它们的蚀变产物,如蛇纹石、滑石、 绿泥石等组成。代表性岩石有纯橄榄岩、橄榄岩、辉石岩和金伯利岩、苦橄岩等。自然界以镁质超基性岩居多。它们常与碱性岩、基性岩共生,形成杂岩体。超基性岩常沿深大断裂带分布,受其控制,形成岩带。岩体的规模大小不一,常呈透镜状、脉状或不规则状。与超基性岩有关的矿产有铬、镍、钴、铂族金属、金刚石、石棉等。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条