1) subchamber
次岩浆房
1.
Metallogenic distribution and mechanism of platinum group elements in the Darwendale subchamber of the Great Dyke,Zimbabwe;
津巴布韦大岩墙Darwendale次岩浆房铂族元素成矿分布和成矿机制探讨
2) magma chamber
岩浆房
1.
The stability of the magma chamber under Wudalianchi modern volcanoes;
五大连池新期火山岩浆房动力稳定性探讨
2.
The tectonic characters of deep layer and high abnormal thermal-flow of Songliao Basin show that the crust low-velocity and high-conduction zone in the deep layer of Songliao Basin may be the magma chamber accumulated in the mid or lower crust and produced from the partly melting inside mantle under the interaction of crust and mantle.
根据松辽盆地深部地质结构、异常高的热流值等特征,认为对松辽盆地深层的壳内低速高导体可以有两种解释:①上地幔发生部分熔融,析离出来的流体相在静压力作用之下上升并穿过莫霍面后,在下地壳上部或中地壳内聚集而成的岩浆房;②在缺水条件下,高热流值作用形成的壳内熔融体。
3) two magma chambers
双岩浆房
4) magma house in crust
壳内岩浆房
5) Magma chamber process
岩浆房过程
6) zonal magma chamber
带状岩浆房
1.
The zonal magma chamber is dominated by dacitic magma with a layer of rhyolitic magma rich in SiO 2 and K on the top, and a little latitic magma in the bottom.
建立了以英安质岩浆为主，顶部有一层富ＳｉＯ２、富Ｋ的流纹质岩浆，底部为少量粗面安山质岩浆的带状岩浆房。
补充资料：直房
1.当值办事之处。
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