1) intrusive rock belt
侵入岩带
1.
Petrology and geochemistry of an active continental-margin intrusive rock belt on the northern margin of the Tarim plate;
塔里木板块北缘活动陆缘型侵入岩带的岩石学与地球化学
2) alkali rich intrusive rock belt
富碱侵入岩带
1.
Altun region of southern Xinjiang are the Yanshanian Lapeiquan Yitunbulak,the Yanshanian Beilisai Abulash and the Himalayan Gez Taxkorgan alkali rich intrusive rock belt which is the youngest alkali rich intrusive rock belt in China.
在新疆南部的昆仑山 -阿尔金山地区 ,分布有三条富碱侵入岩带 ,它们是拉配泉 -伊吞布拉克富碱侵入岩带、别里赛 -阿布拉斯富碱侵入岩带及盖孜 -塔什库尔干富碱侵入岩带。
3) intermediate acid intrusive rock
中酸性侵入岩带
4) volcanic-intrusive rock belt
火山-侵入岩带
1.
Lancangjiang volcanic-intrusive rock belt lies in the middle southern segment of the western Yunnan province, the middle Lancangjiang River, the western border of the Lanping basin and the Simao basin, whose range includes the narrow and long zone of the stream-valley along the Lancangjiang River form Lanping to Simao of Yunnan province which almost presents the southern-northern direction.
云南澜沧江火山-侵入岩带位于云南省西部澜沧江流域中南段,兰坪盆地和思茅盆地之西缘,范围包括自兰坪到思茅的沿澜沧江河谷及两岸大致呈南北向分布的狭长地带。
5) Huashan-Guposhan intrusive belt
花山-姑婆山侵入岩带
1.
Ziucon U-Pb age framework of Huashan-Guposhan intrusive belt,western part of Naniing Range,and its geological significance.;
南岭西段花山-姑婆山侵入岩带锆石U-Pb年龄格架及其地质意义
6) irruptive rock body
侵入岩体
1.
Traditionally,various subphase belts for irruptive rock body are studied and analyzed by mainly drilling well and coring.
侵入岩体油气藏是火成岩油气藏的重要类型之一。
补充资料：绿岩带
| 绿岩带 greenstone belt 蚀变或变质的基性火成岩带。通常指前寒武纪地盾中呈条带状分布的变质基性岩地区，如太古绿岩带等。一个绿岩带中可含有一层或几层基性火山-沉积变质产物。主要岩石类型有细碧岩、玄武岩、辉长岩和辉绿岩等。因变质作用生成的绿泥石、绿帘石、阳起石等矿物促使岩石普遍具有暗绿色。一套完整的绿岩地层，由早期的火山岩和晚期的以浊流沉积为主的碎屑沉积岩或火山碎屑沉积岩组成；火山岩下部以超基性-基性岩为主，并含有一层科马提岩（指一种超基性喷出岩），上部为钙碱性火山岩。 |
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