1.
Sr,Nd AND Pb ISOTOPIC CHARACTERISTICS OF EARLY CRETACEOUS BASALTIC ROCKS FROM THE COAST OF ZHEJIANG AND FUJIAN: EVIDENCES FOR ANCIENT ENRICHED MANTLE SOURCE
浙闽沿海早白垩世玄武岩锶、钕、铅同位素特征——古老富集型地幔的证据
2.
Geochemistry of Early Cretaceous Basalt in the Xiaotian Basin,North Huaiyang Region: Evidence of Enriched Mantle
北淮阳晓天盆地早白垩世玄武岩地球化学:富集地幔的证据
3.
The Concentration Mechanism of Gold in the Crude Oil from Jiyang Depression and Its Relationship with the Mantle Fluid;
济阳坳陷原油中金的富集机理及其与地幔流体的关系
4.
According to the characteristics of trace elements and isotope, the source of the basalt is similar to the OIB source.
微量元素和同位素特征显示,玄武岩起源于与洋岛玄武岩源区相似的富集地幔源。
5.
The composition of mantle is mostly oxygen and silicon, accompanied by iron and magnesium as the most abundant metallic ions. Peridotite is probably the main material making up the mantle.
地幔的成分主要是氧、硅，并伴有丰富的铁和镁金属离子，橄榄岩可能是构成地幔的物质。
6.
Owing to ultramafites coming from mantle, it contains abundant deep information of geology.
超镁铁质岩体由于来自地幔,而含有丰富的深部地质信息。
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.
It was a large, stately apartment, with purple chairs and curtains, a Turkey carpet.
那是间富丽堂皇的大屋子，有紫色的椅子和帷幔，一条土耳其地毯。
9.
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。
10.
The Chemical and Isotopic Compositions and Their Origin of Upper Mantle Volatiles in Eastern China;
中国东部上地幔不同类型流体组成及其性质
11.
Enrichment Regularity and Mechanism of Dispersed Elements Cd, Ge and Ga of Typical Lead-Zinc Deposits in the Eastern Edge of Kangdian Axis;
康滇地轴东缘典型铅锌矿床分散元素镉锗镓的富集规律及富集机制
12.
An ornamental hanging of rich fabric, as behind an altar.
幔布祭坛后面等地的幔布
13.
Ages of Peridotitic Xenoliths from the Central and Eastern Areas of North China Craton and Mantle Heterogeneity
华北克拉通中东部典型地区橄榄岩捕虏体年龄及地幔不均一性
14.
Cenozoic Potassic Volcanic Rocks and Mantle Xenoliths in Maguan, Southeastern Yunnan: Geochemical Characteristics and Implications for Lithospheric Dynamics;
滇东南马关地区新生代富钾火山岩和幔源包体的地球化学特征及其深部动力学意义
15.
Discussion on the Feasible Path to Sustainable Development of Poor and Resource Concentration Areas
资源富集型贫困地区可持续发展路径探讨——以云南省兰坪县为例
16.
Therefore, the CMB is the beginning and the end of whole mantle convection.
因此,地幔底层既是全地幔对流的起点,又是全地幔对流的终点。
17.
In mantle convection models, the mantle viscosity is generally assumed constant or dependent on depth.
粘度为常数或仅随深度变化是地幔对流模型中常用的假设.
18.
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