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物质部分
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     The two parts of existing forms of matter are corresponding to their energy_momentum tensors,respectively. So the total energy_momentum tensor of matter can be expressed as T μν =T (Ⅰ) μν +T (Ⅱ) μν ,where T (Ⅰ) μν and T (Ⅱ) μν are energy_momentum tensors of pure matter part and pure gravitational field part,respectively.
     物质质量 (能量 )这两种形式各自对应着相应的能量 动量张量 ,物质总的能量 动量张量可表示为Tμν =T(Ⅰ )μν +T(Ⅱ )μν ,这里 ,T(Ⅰ )μν ,T(Ⅱ )μν 分别代表物质纯物质部分和纯重力场部分的能量 动量张量 .
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     Their Sr/Y-Y and Ni-Cr relationship coincides with partial melting curves of MORE leaving a 10% garnet amphibolite or eclogite, that shows they were derived from partial melting of oceanic crustal under mantle upwelling and regional extension.
     它们的Sr/Y-Y和Ni-Cr关系与残余10%榴闪岩或榴辉岩的MORB熔融曲线大致吻合,表明它们是地幔上隆、区域拉伸环境下洋壳物质部分熔融的岩浆产物。
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     Sr-Nd-Pb isotope characteristics show that the intermediate-acidic magma roots in an intermixed source of enriched mantle metasomatized by fluid in subduction belt and continental crust.
     Sr—Nd—Pb同位素特征表明岩浆来源于受俯冲流体交代的富集地幔和地壳物质部分熔融的混合源区。
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     The Mesozoic granites and diorites are characterized by strong LREE enrichment and negative anomalies of HFSE (Nb, Ta, P and Ti).
     中生代花岗岩和闪长岩表现出明显的高场强元素(Nb、Ta、P和Ti)负异常以及显著的LREE富集。 εNd(t)值很低(-19.2 --15.3),同样是由古老地壳物质部分熔融形成。
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     RESULTS:Cytotoxicity (IC 50 5.2μg·ml -1 ) was detected and a polysaccharide was found to be a main composition of the high molecular part,which was composed of xylose,mannose,fructose and so on.
     结果:牛膝水提取物的高分子物质部分有细胞毒性,IC50值为5.2μg·ml-1。 多糖为其主要成分,由木糖、甘露糖和果糖等单糖做成。
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     The academic substance culture is the visible part of the academic culture.
     学校物质文化是学校文化的有形部分
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     It has laid the mass foundation for the Yanshanian mineralization.
     这为燕山期成矿作用奠定了部分物质基础。
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     Part II
     第二部分
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     On Substance
     论物质
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     Introductory part.
     导言部分
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  material part
Novel measuring approach for damage of viscoelastic material (Part I): Constitutive model
      
Novel measuring approach for damage of viscoelastic material (Part II): Experiment and numerical calculation
      
Creep crack growth in an elastic-creeping material Part I: mode III
      
Creep crack growth in an elastic-creeping material Part II: mode I
      
Doctoral Dissertation, Rutgers, New Brunswick, New Jersey, 1995); and (iii) inalienable nouns, which also have an inherent relation, defined as a material part-whole relation (Link, Algebraic semantics for linguistics and philosophy.
      
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In 1980—1981 magnetotellurie sounding (MTS) was carried out jointly by the Chinese and French geophysicists along a profile from Lhozha to Yangbajin in Tibet. In the northern part of the profile an intracrust low-resistivity layer was detected at depths of 20—30 km, and in its southern part another low-resistivity layer was found at relatively shallow depths. This paper discusses the characteristics of the telluric currents of the area and the origin of the low-resistivity layers. It is considered that the low-resistivity...

In 1980—1981 magnetotellurie sounding (MTS) was carried out jointly by the Chinese and French geophysicists along a profile from Lhozha to Yangbajin in Tibet. In the northern part of the profile an intracrust low-resistivity layer was detected at depths of 20—30 km, and in its southern part another low-resistivity layer was found at relatively shallow depths. This paper discusses the characteristics of the telluric currents of the area and the origin of the low-resistivity layers. It is considered that the low-resistivity layer in the north might be produced by partial melting of granitic material within the earth's crust, while that in the south might be caused by partial melting of granitic material and water-saturated rocks near a gentle-dipping fault (friction) surface. According to the distribution of subsurface resistivity and temperatures, it is inferred that in the area a relatively low-temperature and high-resistivity massif might be subducted northwards beneath a relatively high-temperature and lowresistivity massif.

1980—1981年中法两国的磁大地电流工作者在西藏洛扎一羊八井地区进行了磁大地电流测深。在剖面的北部深20—30公里处发现一壳内低阻层,在南部还发现一个埋藏深度较浅的低阻层。文中阐述了该区的地电特征,对低阻层的成因进行了探讨。认为北部低阻层是由壳内的花岗岩类物质的部分熔融所引起;南部低阻层的情况较复杂,它可能是由一缓倾角的断层摩擦面附近的花岗岩类物质的部分熔融及饱含热水的岩层所引起。根据地下电阻率及温度的分布推测该区可能有一个温度较低的高阻地块向北俯冲到温度较高的低阻地块之下。

From studies on geological distinctions, metallization and genetic type of the auto-clastic subgranitic porphyry in Xiling tin deqiu. Sn content of the rock, which is a fa-ctcrized by hidden explosion, and the magma resulted from partial melting of upper mantle and lower crust as proposed by Xu Keqin. Sn content of the rock, which is a fa-vorable Sn-bearing rock as indicated by petrochemical parameters, is 10-22 times as high as that of ordinary granites. Close relationship between diagenesis and minero-genesis...

From studies on geological distinctions, metallization and genetic type of the auto-clastic subgranitic porphyry in Xiling tin deqiu. Sn content of the rock, which is a fa-ctcrized by hidden explosion, and the magma resulted from partial melting of upper mantle and lower crust as proposed by Xu Keqin. Sn content of the rock, which is a fa-vorable Sn-bearing rock as indicated by petrochemical parameters, is 10-22 times as high as that of ordinary granites. Close relationship between diagenesis and minero-genesis is verified by Pb isotope ratio. The tin deposit is classified as porphyry depo-sit in view of the common origin of the deposits and the antoclastic subgranitic porphy-ry. Favorable structure for metallization is the contact-zone as well .as explosive breccia.

作者研究了西岭锡矿床自碎次花岗斑岩岩体的地质特征、含矿性、成因类型。认为自碎次花岗斑岩具有隐爆特征。岩浆来自上地幔至下部地壳物质的部分熔化,属于徐克勤教授所划分的过渡型地壳同熔型花岗岩类。岩体中锡含量是一般花岗岩类的10—22倍,并具有含锡岩体的有利岩石化学条件,铅同位素比值证实了成矿与成岩的紧密联系。锡矿床与自碎次花岗斑岩是同源的,应为斑岩型锡矿床。接触带和爆破角砾岩带是成矿的有利构造部位。

Hannorpa Basalts, located at the north of Zhangjiakou,Hebei Province consist of two kinds of basalts of different chemical compositions. These, two kinds of basalts are interbeded and closely associated with each other, and thus give rise to a lithological cycle marked by regular variation in compositions. The characteristic values and the types of distribution of the rare earth elements in both two kinds of basalts show different features but possess a regular variation. They are all the partly melted products...

Hannorpa Basalts, located at the north of Zhangjiakou,Hebei Province consist of two kinds of basalts of different chemical compositions. These, two kinds of basalts are interbeded and closely associated with each other, and thus give rise to a lithological cycle marked by regular variation in compositions. The characteristic values and the types of distribution of the rare earth elements in both two kinds of basalts show different features but possess a regular variation. They are all the partly melted products of upper mantle materials. The calculation with the formula of part-melting quantitative model suggests that the alkaline basalts and the tholeiitic basalts are the lower grade partly melted products of garnet iherzolite (the lower level)and spinel iherzolite (the overling level) respectively in the upper mantle.

位于中国河北省张家口以北的汉诺坝玄武岩,由两类岩性不同的玄武岩组成,它们相间成层、相伴互生,构成变化规律的岩性旋回。两类岩石的一系列稀土元素特征数值和分配型式都表现出既不相同又有变化规律的特征。它们都是上地幔物质部分熔融的产物,据部分熔融定量模式计算认为,本区碱性系列玄武岩和拉斑系列玄武岩分别是上地幔处于不同部位的,既较深处的榴石二辉橄榄岩和其上部的铬尖晶石二辉橄榄岩的低度熔融的产物。

 
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