1.
Late Mesozoic Magmatic Intrusion Sequences Implication for the Transition of Tectonic Regimes, Central of the Dabie Orogenic Belt, China;
大别造山带核部晚中生代岩浆侵位序列与构造体制转换
2.
Magmatic emplacement is a complex physical chemical process which controls spatial distribution of rock body and deposit.
岩浆侵位过程是一个复杂的物理化学过程,控制着岩体和矿床的空间分布。
3.
Ore-forming specialty of the tectono-magmatic zone in Nanling region and its emplacement dynamics for metallogenic series of W-Sn polymetallic deposits
南岭钨锡多金属矿床成矿系列与构造岩浆侵位接触构造动力成矿专属
4.
The rock mass produced by an intrusive process.
侵入岩浆岩浆侵入过程中生成的岩块
5.
THE GEORHEOLOGICAL CHARACTERS AND GEOTECTONIC ENVIRONMENTS OF THE ASCENT AND EMPLACEMNT OF GRANITIC MAGMA IN THE LIMU-YUANSHISHAN DISTRICT,GUANGXI
栗木—圆石山地区花岗岩浆的地质流变学特征和侵位定位环境
6.
EMPLACEMENT AGE OF GRANITIC MAGMA IN THE YULONG PORPHYRY COPPER BELT, EASTERN TIBET
论藏东玉龙斑岩铜矿带岩浆侵入时代
7.
Proterozoic basaltic magma intrusion event in the Altai ,Xinjiang
新疆阿尔泰元古代基性岩浆侵入事件
8.
Magma Intrusion in No.2 Mine in Xuandong Influence on Gas Existence
宣东二矿岩浆侵入对瓦斯赋存的影响
9.
The heat and pressure from igneous intrusion cause the alteration of surrounding rocks.
入侵岩浆的热能和压力导致了围岩的变化。
10.
The Study of Interpretation Methods 3D Seismic and Its Application on Magmatic Intrusive Mass;
岩浆岩侵入体三维地震解释方法及应用研究
11.
A new type of magmatic rock orientation mechanism:screw upwelling
岩浆岩定位机制的新类型——螺旋上冲
12.
We will make certain assumptions about the properties of the intruding magma and of the intruded strata.
我们对入侵的岩浆和被侵入地层的性质做某些假定。
13.
Ore-bearing rock body is located at the top of" magma tree" within the belt of dimicaceous granite-granitic pegmatite.
含矿岩体位于“岩浆树”顶端-二云母花岗岩-花岗伟晶岩带。
14.
THE GEOLOGICAL CHARACTERISTIC AND EMPLA-CEMENT MECHANISM OF INTRUSIVE ROCK DURING CALEDONIAN OROGENY IN XIAO QINLING MOUNTAIN
小秦岭加里东期侵入岩地质特征及侵位机制
15.
Not all molten rock cools on the earth's surface. Some magma cools beneath the surface after having been injected or intruded into the rocks of the earth's crust.
并非所有的熔融岩石都是在地表冷却的，一些岩浆在侵入地壳岩石中之后，在地表之下冷却成岩。
16.
The Mesozoic and Cenozoic plutonic intrusive rocks are grouped into the Lhagoi Kangri and Gangdise granite zones.
将中新生代深成侵入岩划分为拉轨岗日花岗岩带和冈底斯花岗岩带两个岩浆带;
17.
Structural pattern and intrusion mechanism of the Banshanpu massif in eastern Hunan
湘东板杉铺岩体构造样式与侵位机制
18.
When you see a termination of a sill you should ask yourself how the intruding magma behaved at the moment of intrusion.
当你看到岩床终端时你应该自问，侵入的岩浆在侵入期是如何表现它们的特征的。