rock magma

Igneous Rock , rock formed when molten or partially molten material, called magma, cools and solidifies.

火成岩是熔化或部分熔化的物质(岩浆)经过冷却固化形成.

Sometimes magma reaches the surface through volcanoes. Then the molten rock is called lava.

当岩浆通过火山口溢出地表时, 便可称这种熔融的岩石为熔岩.

Igneous rock the passionate magma is in ground or is in the earth's surface condensation formation rock from ground profundity.

火成岩由地下深处炽热的岩浆在地下或在地表冷凝形成的岩石。

Igneous rock is rock formed by solidification from a molten state; especially from molten magma.

火成岩是从熔融状态(特别是通过熔化岩浆)凝固而成的 石头.

Their petrological and geochemical characters suggest that the host rock of the xenoliths is basanite, and the magma has not experienced obvious differentiation and assimilatory contamination.

岩石学和地球化学特征揭示包体寄主岩为碧玄岩，岩浆没有经历明显分异和同化混杂作用。

Ultrabasic rock alkali olivine basalt magma

超碱岩，超基性岩碱性橄榄玄武岩岩浆

Deep beneath the Earth's crust there are pockets of partially liquid rock called magma.

在地壳的深处有很多异体囊,囊中有半液态的岩叫作岩浆.

This paper elaborates area sediment construction, magma evolutions, background of mineralization structure, mineral deposit mineralize rock body scale, shape and produce form, rock body invade each and invade looks, mineral deposit origin cause of formation and ore type and characteristic in all-round way;

本文对金川铜镍矿区区域沉积建造、岩浆演化、成岩成矿构造背景、矿床成矿岩体规模、形态与产状、岩体侵入期次及侵入相、矿床成因与矿石类型及特征进行了全面阐述；

The molten rock within was released in a jet of gas and fragmented magma.

内部的熔岩随着喷射的气体和碎裂的岩浆喷涌出来.

There is obviously fault contact between the cap rock and Archeozoic rock basement, associated with basic magma intrusion and with the characteristics of the back margin tensile of d é collement structure.

盖层与太古代基底之间存在明显的断层接触，并伴随基性岩浆侵入活动，具有滑脱构造后缘拉伸带的特征。