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岩浆

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The paper described the influences of source-rock, magmatic hydrothermal fluid, biologic sedimentation, and groundwater on the enrichments of associated elements in coal.

分析了陆源作用、岩浆热液作用、沉积的生物作用、深循环热液流体作用等对煤中伴生元素富集的影响。

By using quantum statistics,this paper obtains the calculation formula of entropy of phonons and initial results,and points out that the entropy of phonons plays an important role in the associated reaction of two kinds of anion structural groups in silicate melts.

熔体阴离子结构团缔合过程中声子熵的研究何安明李秉新石焕文(西安地质学院,西安710054)关键词熔体阴离子结构团缔合声子熵近年来,中外学者已经开始重视对岩浆熔体的物理过程和机制(如利用喇曼光谱直接测定硅酸盐熔浆的结构等)的研究工作,并取得了重要进展。

Available good quality age dates and zircon Hf isotopic data suggest that the northern parts of the Gangdese experienced a zonal magmatic flareup with strong input of mantlederived materials at ~110 Ma.

已有高质量年龄数据和锆石Hf同位素指示冈底斯带中北部地区在大约110 Ma发生了带状岩浆大爆发并伴随着幔源物质显著增加。

This shows that the granites both in the HP and UHP metamorphic rocks have a common magma source.

这表明高压变质岩系和超高压变质岩系中的面理化花岗岩具有相同的岩浆来源。

A lot of granites and volcano bodies were formed.

岩浆活动强烈而广泛,形成了大量的花岗岩和火山岩。

The results show that the Dangchuan and Shimen granites have magma crystallization ages of 438±3 Ma and 220±2 Ma, respectively.

结果表明,党川花岗岩和石门花岗岩的岩浆结晶年龄分别为438±3Ma和220±2Ma。

In this paper, we introduce the controlled factors of weathering of granites and the characteristics of the major granite landscapes. The mechanism of these landscapes are outlined.

由于其不同大地构造背景,产生了不同的岩浆成分和结构构造以及不同的断裂型式(Pitcher,1983);同时也由于所处的不同的气候环境,导致了花岗岩地貌具有不同的类型。

It is suggested that the ore deposit under study was relative to the mixing of the lowtemperature and hightemperature hydrothermal solutions.δ18O and δD values of oreforming fluid of different ore bodies are unanimous, thus indicating that fluid homogenisation once happened before the formation of oreforming fluid.

研究结果表明,该矿床的形成与中低温热液与中高温热液的混合有关;成矿流体的H、O同位素组成在不同矿体中没有明显的差别,流体形成前曾存在流体的均一化作用;成矿流体的形成是地层循环水与变质水、岩浆水在流体储库中充分混合的结果。

When in the sedimentary formation these living thing chemical energy material, arrives between the earth's crust and the mantle rock magma region, because receives the high temperature high pressure the function, can the instantaneous aggravating internal heat response degree, also because these biological energy material stratum distributes non-uniform, thus has further created the partial region superheat, then intensified the profile conduction and the instantaneous paroxysm, finally intensified earth's surface and so on the earthquake volcano as well as plate movement terrain changes.

当沉积地层内的这些生物化学能物质,到达地壳与地幔之间的岩浆区域,由于受到高温高压的作用,就会瞬间加剧内热反应的程度,又由于这些生物能物质的地层分布不均匀,从而进一步造成了局部区域的过热,进而加剧了波形传导和瞬间爆发性,最终加剧了地震火山以及板块运动等地球表面的地形变化。

Then ,came rocks,magma,floods and mudflows.

然后,岩石,岩浆,和泥石流来了。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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