1.
At the same time, with (he theory of dissipation structure and the views of the earth mantle hot-pillar has been established the pattern of the cause of formation
同时,用耗散结构理论和地幔热柱观点建立了该区火山成因模式.
2.
The Study of the Relationship between Emei Mantle Plume Activity and Zhenfeng Shuiyindong Gold Deposits
峨眉地幔热柱活动与贞丰水银洞金矿床形成关系研究
3.
The material in the center of the column, being the hottest, will rise fastest, and only this hottest material will likely reach the surface.
作为最热的地幔柱中心的物质将上升得最快，并且只有这最热的物质才有可能达到地幔的表面。
4.
New seismic constraints on the upper mantle structure of the Hainan plume
海南地幔柱上地幔结构新的地震学约束
5.
An upwelling of molten material from the earth's mantle.
地柱从地幔隆起的一段熔化物
6.
Temporal Variation in Volume Flux of Hawaii Plume through 35 Ma
Hawaii地幔柱近35Ma的体积流量变化
7.
The Mantle Plume Model for the Evolution of Bohai Bay Basin
渤海湾盆地构造演化的地幔柱模型研究
8.
Discussion about mantle plume in southern Hunan with its geological significance
浅谈对湘南地幔柱构造的认识及其地质意义
9.
Plumes are hot enough to melt their way through the ocean floor or through a continent.
地幔羽的热量足以熔穿海底或大陆。
10.
There is a higher heat production in the upper mantle below oceans than below continents.
大洋下的上地幔要比大陆下的上地幔有较高的热产率。
11.
S-type granites should not be considered as the evidence of plume magmatism.
不能把S-型花岗岩作为地幔柱岩浆作用的证据。
12.
Preliminary Discussion of the Relation Between Mantle Plume Structure of Emei Mountain and Uranium Mineralization of Guizhou
峨眉山地幔柱构造与贵州铀成矿关系初探
13.
Simulates on Melting, Elastic and Thermodynamic Properties of Major Material of the Lower Mantle;
下地幔主要矿物的熔化、弹性和热力学特性研究
14.
ARCHEAN GEOTECTONIC TRANSITION OF SYSTEMS FROM MANTLE PLUME TO PLATE TECTONICS IN NORTH CHINA
华北太古宙从地幔柱体制向板块构造体制的转化
15.
Characteristics of Plume-Related A-Type Granites:An Example from the Emeishan Large Igneous Province
与地幔柱有关的A型花岗岩的特点——以峨眉山大火成岩省为例
16.
Each plate consists of a section of the earth's crust and a portion of the mantle, the thick layer of hot rock below the crust.
每个板块由一段地壳和一部分地壳下部厚层炽热岩石地幔组成。
17.
Plumes are generally believed to form over localized hot spots deep within the mantle layer.
地慢羽一般被认为是形成于地幔层内部深处固定的热点上。
18.
The plates move slowly and continuously on the atmosphere, a layer of hot, soft rock in the mantle.
板块缓慢连续地在软流圈上移动，该软流圈是指地幔中炽热柔软层。