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The vibration energy or the electronic and vibration entropy of the gaseous molecules are approximately used as the energy or entropy of the solid. In this approximation, thermodynamic functions 、、 and hydrogen isotopes equilibrium pressure of the hydrogenating reaction have been calculated .Then we can fit the relations between temperature and equilibrium pressure.

在ZrH2的E和S的过程中,以气态分子总能量中的振动能EV代替该分子处于固态时的振动能量E,以电子和振动熵SEV代替分子处于固态熵的近似方法,计算了不同温度下金属Zr与氢同位素反应的,和以及氢化反应平衡压力,并导出了氢化反应平衡压力与温度的关系。

But if the suspect were in Las Vegas, which has adifferent signature, he could find himself nicked.

但是如果嫌犯曾经在拥有不同同位素特征的拉斯维加斯,他就会露出马脚。

The contrasting isotope data between 850 Myr ago and the Neoproterozoic suggest that the terrestrial expansion of photosynthesizing communities preceded the significant climate perturbations of the late Precambrian glaciations, and was followed by a rise of O2 ref.

对比850百万年前和新元古代的同位素数据表明陆地光合作用群落生物的爆发应当先于晚前寒武纪冰川作用的气候变动。

Based on detailed geological observation and precise dating of porphyries in combination with data available, the authors hold that the Indosinian porphyries in the Zhongdian island arc zone can be divided into two parts, i.

在较为详细的野外地质观测和精确的同位素测年的基础上,结合前人资料,将中甸地区的印支期岛弧斑岩体分为东、西两个斑岩带,东斑岩带形成于 2 1 8~ 2 0 3Ma ;西斑岩带形成于 2 4 2 。92~ 2 37.5Ma。

The sulfur and lead isotope compositions indicate that the ore_forming materials were mainly derived from the volcanic rocks and granodioritic porphyries.

硫_铅同位素指示成矿物质主要源于火山岩地层和花岗闪长斑岩脉。

Based on detailed geological observation and precise dating of porphyries in combination with data available, the authors hold that the Indosinian porphyries in the Zhongdian island arc zone can be divided into two parts, i.e., the eastern porphyry belt formed during 218~203 Ma and the western porphyry belt formed during 242.92~237.5 Ma.

在较为详细的野外地质观测和精确的同位素测年的基础上,结合前人资料,将中甸地区的印支期岛弧斑岩体分为东、西两个斑岩带,东斑岩带形成于 2 1 8~ 2 0 3Ma ;西斑岩带形成于 2 4 2 。92~ 2 37.5Ma。喜马拉雅期(5 3.0 2Ma)斑岩叠加于早期的斑岩体之上,与斑岩铜矿化关系密切。

In this his dissertation, the field geological work and modern analysis were finished on the Qulong ore-bearing porphyries. The mineralization chronology, petrology, element and isotopic geochemistry were studied on the porphyries. This dissertation also compare this work in Qulong ore-bearing porphyries with other ore-bearing porphyries in Gangdese belt, in order to probe into dynamical background and mineralization features of the ore belts in the condition of India-Eurasia collision.

在充分搜集、利用前人资料及成果的基础上,本论文力求以地球动力学和现代成矿理论为指导,采用先进的分析测试手段和野外地质工作相结合的方法,通过重点研究驱龙斑岩铜矿床的岩石学、同位素地球化学、常量与微量元素地球化学及成矿年代学,并与冈底斯其它斑岩矿床对比,探讨在印度—欧亚大陆碰撞条件下,冈底斯斑岩铜矿带的大陆动力学背景及成矿规律。

Pb-Sr-Nd isotope tracing shows that the source of magma in the island-arc belt of Zhongdian area belongs to crust-mantle mixed type. The proportion of mantle material is 59.5% crust's is 40.5%. Similarly, for the Cenozoic alkaline-enriched porphyries, the source of magma is crust-mantle mixed type, but the proportion of mantle material is increased to 54.3%.

通过Pb-Sr-Nd同位素示踪,发现中甸地区岛弧带岩浆物质来源为壳幔混合型,印支期的地幔物质的比例m平均值为59.5%,地壳物质的为40.5%;剑川、北衙等地的新生代富碱斑岩的m值平均54.3%,也表现为壳幔混合型,但与印支期火山-侵入杂岩相比,其地壳物质的比例增高。

The δ^34S values of ore minerals vary slightly from -3.1‰ to +0.7‰ with an average value of -1.1‰ and the δ^34S values of the ore-bearing porphyries are -1.4‰ and -1.5‰, indicating that sulfur is mainly derived from the magma of porphyry.

雪鸡坪铜矿S,Pb同位素组成共同指示成矿物质主要来自于深部岩浆,这种岩浆可能主要起源于俯冲洋壳板片的部分熔融并受到少量地壳物质的混染。

Any initial carbonate precipitates are therefore more susceptible to alteration of the C isotope ratio.

因此任何初始的碳酸盐沉积都会容易受到碳同位素比值的交代影响。

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