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1)  small intrusions
小岩体
1.
Results of research indicate that Ni-Cu(PGE)ore deposits hosted in small intrusions in China mainly occur in three geologic settings:(1)within paleo-continents,(2)in orogenic belt,and(3)continental rift system such as the Panxi Rift system where a large number of flood basalts and associated mafic-ultramafic intrusive are present.
文章进一步提出中国小岩体镍铜(铂族)矿床产出于三种地质背景,即古大陆内的小侵入体、造山带内小侵入体和与大陆溢流玄武岩有关的小侵入体,分别介绍了金川、喀拉通克和白马寨三个典型矿床的地质情况。
2.
Small intrusions are small size,shallow buried in the form of cylinder-shape,vein,mushroom-shape,stock and dike,the attitude of small intrusions in general tend to south and southeast with a dip angle of above thirty degrees.
鄂东南燕山期小岩体(群)有137处,主要分布在两大层间顺层滑脱拆离带中和毛铺—两剑桥断裂及其附近。
2)  Minor intrusion
小斑岩体
3)  small instable rock
小危岩体
1.
Usually,there are densely distributed small instable rocks in a low-angled stratofabric rock slope.
缓倾角层状岩质边坡是小危岩体出露的主要坡型之一。
4)  Xiaoheishan pluton
小黑山岩体
1.
The Xiaoheishan pluton is located in the southern Liaodong Peninsula of the eastern North China Craton,and consists of deformed diorite,granodiorite and biotite granite.
小黑山岩体位于辽东半岛南部,由变形的闪长岩、花岗闪长岩、花岗岩组成。
5)  Late stage small massifs
晚期小岩体
6)  intermediate-acid small intrusive bodies
中酸性小岩体
1.
There are many intermediate-acid small intrusive bodies among Yanshanian intrusive rocks and they are usually closed related to Molybdenum-polymetallic mineralization.
在燕山期侵入岩中,中酸性小岩体数量众多,与钼等多金属矿化关系密切。
补充资料:高温岩体发电
      利用地表深层高温干岩体所含的热量发电(见高温岩体电站)。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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