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    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
    A Study on Cr and Ni Deposits in Si-O System from the Mantle
    幔源Si—O系统铬和镍的矿床学研究
    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
    A STUDY ON THE SUITABLE CONDITIONS OF THE MANTLE TISSUE CULTURE OF PEARL OYSTER
    育珠蚌外套膜组织培养适宜条件的研究
    REE AND Sr, Nd ISOTOPE GEOCHEMISTRY OF THE MANTLE XENOLITES FROM HUANGYISHAN BASALT, KUANDIAN, LIAONING PROVINCE
    辽宁宽甸黄椅山玄武岩中地幔岩捕虏体的REE 及 Sr、Nd 同位素地球化学
    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
    The Determination of Trace Element Contents in the Mantle of Ostrea rivularis
    牡蛎外套膜中微量元素含量的测定
    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
    Very high Cr, Ni and low Sc (< 30 μ g/g), TiO2 (< 1% ) contents in the high magnesian ultrapotassic lavas imply the mantle sources of spinel harzburgite.
    较高的Cr、Ni含量和较低的Sc(<30μg/g)、TiO2(<1%)含量暗示了源区为尖晶石相方辉橄榄岩;
    The mantle-derived Helium of all samples averagely occupies the whole Helium about 26.2%, the tiptop about 48.8% which reflect the fault zone is repressing extent structure environment.
    同时所有样品中的幔源氦平均约占总氦的26.2%,最高可达48.8%以上。
    The mantle-derived Helium of all samples averagely occupies the whole Helium about only 2.27%, the maximum about 8.9%.
    而在滇中地区—小江断裂带却是另一番景象,该区样品中的幔源氦平均约占总氦的2.27%,最高也才8.9%。
    A few epithelial cells and haemocytes in the connective tissue of the mantle reveal strong PO positivity. Two kinds of strong PO positive granules in the cytoplasm are about 150-220nm and 350—450nm in diameter.
    外套膜的少数上皮细胞和血细胞中,有直径分别为150—220,350—450 nm的2种颗粒,呈PO强阳性.
    The mantle tissues of clam Ruditapes philippinarum were primary cultured in vitro with Dulbecco's Modified Eagle Medium(D-MEM) and Medium 199(M199). RNA/DNA ratio was used to evaluate the proliferation of cells.
    以D-MEM和M199为基础培养基,对菲律宾蛤仔的外套膜进行了细胞培养,并以RNA/DNA比值作为评价细胞增殖的指标。
    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。
    Sulphur isotope contained in pyrite samples is from 2.1 to 4.4 per mille with a mean of 3.1 per mille and narrow range of data distribution,and concentrated near source-of-the-mantle sulphur. These reflect the features of source-of-the-mantle sulphur isotope.
    黄铁矿样品的σ34S为2.1‰~4.4‰,平均值为3.1‰,数据分布范围狭窄,集中于幔源硫附近,反映了硫的幔源特征。
    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
    Study on some pathogenetic ciliates from the mantle cavity of marine molluscs
    海洋贝类几种危害性纤毛虫的研究
 

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