Magma

The volcano threw new showers of magma and ash into the air .

火山又向空中喷出了岩浆和火山灰。

Most of us , when we talk about volcanoes , think of the classic cone shapes of a Fuji or Kilimanjaro , which are created when erupting magma piles up ．

我们大多数人在谈论火山时,都会想到富士或乞力马扎罗的典型圆锥体形状,它们是在岩浆喷发堆积时形成的。

The enclaves are remnants of rocks which partially melted to form granitoid magma .

包体为部分熔融形成寄主花岗岩岩浆的源区岩石残余。

This paper is an application of the theory of magma dynamics .

本文是岩浆动力学理论的应用。

Magma density , structure and fluid dynamics the second density

岩浆的密度、结构及流体动力学&八十年代火成岩研究新进展

The Characteristic of Thermal Evolution of Magma Intrusion in Hot Spring Area

热泉地区岩浆侵入过程的热演化特征

Differentiation mechanism and evolution of high level magma reservoir from xiangshan , China

相山高位岩浆房分异机制和演化

Structure & magma control of gold mineralization in northwest sichuan

川西北地区金成矿的构造&岩浆控制

Effect of Magma Intrusion on the Thermal Evolution in a Sedimentary Basin

沉积盆地热演化过程中的岩浆作用

Main types of magma sulfide deposits in China

中国岩浆硫化物矿床的主要类型

The ore deposit is the common product of magma , strata and structure .

矿床（体）是岩浆热液、地层、构造综合作用和有机组合的产物。

Open magma system : progress in igneous petrology in 1980 's

开放的岩浆体系&八十年代火成岩研究的新进展之一

Fangshan Pluton : Magma Source , Generation Mechanism and Dynamic Significance

房山岩体的岩浆来源、形成机制及动力学意义

Lead source is mainly from magma .

铅的来源以岩浆源为主，铅同位素组成较均一。

The volcanic rock series has same magma source .

基性火山岩系具有同一岩浆源区。

Geological conceptual model on the copper-nickel sulfide deposits of magma type

岩浆型铜镍硫化物矿床地质概念模型

Ore-forming magma is characterized by low density , low viscosity and high volatile content .

成矿岩浆具低密度、低粘度、富含挥发份的特征；

Magma Evolution and Deep Geological Processes of Early Permian Tarim Large Igneous Province

塔里木早二叠世大火成岩省的岩浆演化与深部地质作用

The other is of mantle - derived magma type .

二是认为属幔源岩浆型花岗岩。

Researchers think it is more probable that the two magma sources are mixing .

研究人员认为，两种岩浆来源互相混合是较有可能的解释。

Vertical Deformation Inversion of Magma Activity in Tengchong Volcanic Area

以垂直形变资料反演腾冲火山区岩浆活动性的初步研究

We call this rock material magma .

我们称这种岩石材料为岩浆。

To examine the chemical variation in the course of crystallization evolution of natural magma ;

查明天然岩浆结晶演化过程中化学成分的变迁规律；

Quaternary Volcanic Activity and Magma Evolution in North Hainan Island

琼北第四纪火山活动与岩浆演化

The Mesozoic volcanic age and the source of magma in South Jiangxi

赣南中生代火山活动时代及岩浆来源

However , magma is a non-Newtonian fluid in most instances .

然而，在大多数情况下，岩浆是一种非牛顿流体。

The REE evidence shows that the magma formation was mainly controlled by partial melting process .

稀土元素反映岩浆形成主要受部分熔融作用控制。

Therefore , the magma is not likely to be found along the anticline .

因此，岩浆的侵位一般不会沿背斜发生。

Isotopic components of two series of Li-F granite derived from different magma sources

不同来源两个系列Li-F花岗岩的同位素组成区别

Studies on a sudden change of light transmissivity of crystal magma at its saturation temperature

晶浆在饱和温度透光率突变的机理研究