1) the Fangshan intrusive body
房山侵入体
1.
By means of numerical simulation, the impact of regional metamorphism on the cooling of the Fangshan intrusive body in Western Hill of Beijing is studied.
通过传热数值模拟分析了区域变质作用对北京西山房山侵入体冷却的影响。
2) Post-volcanic intrusion
后火山侵入体
3) intermediate intruded subvolcanic complex
中性侵入-次火山杂岩体
1.
The Kuoerzhenkuola intermediate intruded subvolcanic complex located in the eastern Sawuershan, the north-western margin of the Zhungaer Basin, Xinjiang, was formed in the Late Palaeozoic Era island arc.
新疆准噶尔西北缘萨吾尔山东部的阔尔真阔腊中性侵入-次火山杂岩体,形成于晚古生代岛弧构造环境。
4) granitic volcano-intrusive complexes
花岗质火山-侵入杂岩体
5) volcano_intrusive rocks
火山-侵入岩
1.
Sr and Nd isotopic composition and material sources of Mesozoic volcano_intrusive rocks in the northern margin of Dabie Mountains;
大别山北缘中生代火山-侵入岩锶-钕同位素组成特征及其物质来源
6) pre-kinematic intrusion
造山前侵入
补充资料：房山
①山墙。②〈方〉泛指房屋四周的墙：前～ㄧ后～。
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