地幔热柱,mantle plume
1)mantle plume地幔热柱
1.The ore-forming materials are mainly derived from the earth core constrained by deep processes and moved up to surface with multi-stages of mantle plume evolution and is contaminated with earth crust materials.认为峪耳崖矿区成矿物质应主要来自地核,受深部过程的约束,成矿物质随地幔热柱多级演化向地表迁移,在其上升过程中,与壳源物质发生部分混染,使所测同位素数据往往表现出以深源为主、并混有少量壳源物质的特征。
2.Mantle branch is the third-grade tectonic unit during multiple evolution of mantle plume.幔枝构造是地幔热柱多级演化的三级单元,其对内生矿产的成矿控矿作用十分明显。
3.Mantle branch structure is the third-order unit of mantle plume multistage evolution.幔枝构造是地幔热柱多级演化的第三级构造单元 ,其核部变质—岩浆杂岩隆起与外围盖层之间的主拆离带体系是很好的成矿控矿构造。
英文短句/例句

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 MaHawaii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。
相关短句/例句

Plume[英][plu:m][美][plum]热地幔柱
3)Sub-mantle plume地幔亚热柱
1.According to the study of mantle plume for ten years,it is concluded that sub-mantle plume is strongly uplifting under fault basin of North China.笔者依据近十余年华北地幔亚热柱的研究认为 ,华北断陷区之下为一强烈上隆的地幔亚热柱。
4)mantle plume(hot spot)地幔柱(热点)
1.These magmatic rocks,including basic,intermediate,intermediate-acid,acid and alkaline rocks,came from earth s crust and mantle and these both and were controlled by the mantle plume(hot spot).这些岩浆岩有基性、中性、中酸性、酸性和碱性,它们来自幔源、壳源、或壳幔混源,是地幔柱(热点)控制出现的热岩系。
5)hot-spot plume热点地幔柱
6)mantle plume and hotspot地幔热柱和热点
延伸阅读

地幔地幔earthmantle地壳和地核之间的中间层。平均厚度为2800余千米。1914年B.古登堡根据地震波走时测定地核的深度为2900千米,比现代精密测量的结果只差15千米。因此,地核-地幔边界又称古登堡不连续面。见地球内部构造。