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地幔
    Chronology and Geochemistry of Mafic Rocks from Fujian Province: Implications for the Mantle Evolution of SE China Since Late Mesozoic
    福建省基性岩的年代学和地球化学:晚中生代以来中国东南部地幔演化
    THE RELATIONSHIP BETWEEN THE GRAVITY FIELD AND THE STRESS FIELD OF THE MANTLE CURRENT
    重力场和地幔流应力场的关系
    TYPES OF MELTING RESIDUE AND STRUCTURAL DEFORMATION OF THE MANTLE PERIDOTITE BODIES IN OROGENIC BELT OF CHINA
    中国大陆造山带中地幔橄榄岩体的熔融残余类型及其构造形变
    STANDARDIZATION CALIBRATION OF THE MANTLE WAVE MAGNITUDE AND OBSERVATIONS
    地幔波震级的规范化标定与观测
    REE CHARACTERISTICS OF PARTIAL MELTS IN THE MANTLE PERIDOTITE FROM SHUANGGOU, YUNNAN PROVINCE
    云南双沟地幔橄榄岩中部分熔融物的REE特征
    GLOBAL SEISMIC TOMOGRAPHY, THE DENSITY HETEROGENEITY OF THE MANTLE AND CONTINENTAL DYNAMICS
    全球地震层析地幔密度横向不均匀及大陆动力学
    Initial n(187Os)/n(188Os)rate is 1.127±0.043,which suggests that the ore-forming materials originated from the crust,but not from the mantle.
    等时线的初始n(187Os)/n(188Os)值为1.127±0.043,指示成矿物质来源于地壳而不是地幔
    The calcite of uranium deposit has δ 13C values of -8.5 ~ -3.1‰, which coincides with the mantle δ 13C values (-5±2‰).
    矿床中方解石δ~(13)C值为-8.5~-3.1‰,相似于地幔值(-5±2‰);
    ANALYSIS OF THE THERMODYNAMIC UNSTABILITY IN THE MANTLE
    地幔热力不稳定性分析
    THE RELATIONSHIP BETWEEN THE ORIGIN OF ALKALINE-ULTRABASIC COMPLEX AND THE MANTLE IN FAR EAST AREA OF RUSSIA
    俄罗斯远东地区碱性-超基性杂岩体成因与地幔之关系
    Geochemical characteristics of precious metallic elements in the mantle peridotite from the Luqü ophiolite,Tibet
    西藏路曲蛇绿岩地幔橄榄岩的贵金属元素地球化学特征
    THE MANTLE CHARACTERISTICS OF QUATERNARY CONTINENTAL LITHOSPHERE,SOUTHEAST COAST OF CHINA
    东南沿海地区第四纪大陆岩石圈地幔的特征
    Seismic anisotropy in the mantle transition zone beneath Fiji-Tonga
    斐济—汤加地幔过渡带的地震波各向异性
    Mesozoic-Cenozoic Mafic Magmatism in Western Shandong Province and Its Implication for the Chemical Evolution of the Mantle
    鲁西中、新生代镁铁质岩浆作用与地幔化学演化
    The Native Iron and Wustite Assemblage: Records of Oxygen Element from the Mantle
    记录地幔中存在氧元素的自然铁-方铁矿组合
    Mineralogical Deduction of Characteristics of the Mantle Beneath North Hetian Area
    和田地区北部地幔特征的矿物学反演
    STUDY ON THE MANTLE ANISOTROPY IN CHINA MAINLAND BY USING SHEAR WAVE SPLIT
    利用剪切波分裂研究中国大陆上地幔各向异性
    An Explanation of Correlation between Hydrothermal Heat and ~3He in the Mantle
    对地幔热流和~3He相关性的解释
    The Ar-He analytical results show that 3He/4He ratios of fluid inclusions in pyrite are 1.05~3.17R/Ra, 100 times higher than that of the crust and markedly lower than that of the mantle.
    黄铁矿流体包裹体的3He/4He比值为1.05~3.17R/Ra,高于地壳的3He/4He 比值100 余倍,但明显低于地幔流体的3He/4H e比值;
    The velocity at the top of the mantle is about 7.8 km/sec.
    其特点为:上地幔顶部的速度为7.8公里/秒;
 

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