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作者研究
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  author ' s study
    Based on the author's study it is indicated that byusing a combination of API analogue approach and Waring Blender's mixing method, optimal results will be obtained.
    经作者研究表明,以API模拟法和waring Blender搅拌法配合使用效果最佳.
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  “作者研究”译为未确定词的双语例句
    The author select rock mass from damsite in Laxiwa hydroelectric station as object to which information processing system on rock mass structure is applied.
    以拉西瓦水电站坝址工程岩体作为作者研究的岩体结构信息处理系统的应用对象,野外快速拍摄,室内准确高效的采集完成岩体结构工程要素。
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    A new approach based on microscopy has been developed to determine theangle of inclination(θ) for the plane-law twin composition plane(010) of albitein the plagioclase slice obliquely cut along[010] crystal zonc.
    本文作者研究出来的测定Np′∧[010]_(max)的新方法,以测定斜长石斜切[010]晶带切片中钠长石面律双晶结合面(010)的倾角(θ)为手段,按a=90°-θ公式求出斜切[010]晶带切面的倾角(a)。
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    In 3D display, this paper discusses the projection display method, analyzes and compares the merits and shortcomings of some display methods, such as projection display, entity display and Virtual-Reality display and so on.
    在三维显示中,本文作者研究了投影显示法,并分析比较了投影显示法与实体显示法及虚拟现实显示法的优缺点;
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    The Middle Jurassic flora in Western Hills of Beijing also includes Mentougou florain Chenfen, Douyawei, Huangqisheng (1984) and Zhaitang flora in Duanshuying (1987)by comparison.
    经对比分析,作者研究的植物群与陈芬、窦亚伟、黄其胜(1984)研究的门头沟植物群和段淑英(1987)研究的斋堂植物群同为北京西山中侏罗世植物群的组成部分。
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    There are high content of Pb、 Zn and organic matter in the wall rack of the deposit and the upper Paleozic stratum, which would provide substance for ore-forming by the movement of later rainwater and mixed themic water.
    前人资料和作者研究表明,围岩及上覆古生界地层含有较丰富的Pb、Zn及有机质,为后期雨水热液及混合热液活动成矿提供了物质基础。
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  author ' s study
Three others seen at this institution outside the time frame of the author's study have also been included.
      
This paper seeks to improve knowledge of ecological resources within the DMZ by combining and synthesizing the author's study results with the outcome of surveys of the DMZ conducted by various organizations.
      
Summarized is the author's study of the ocean circulation dynamics with numerical models, for which he was honored by the Okada Prize (1979).
      
This article reviews the author's study on waves in planetary fluids for which the Okada Prize of the Oceanographical Society of Japan was awarded in 1981.
      
This article reviews the author's study on the instability and nonlinear evolution of density fronts and boundary currents, for which the Okada Prize was awarded in 1990.
      
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The work of certain previous authors indicates that in the crust of China, intensive horizontal stresses exist as a result of the compression from the east by the Pacific Plate and by the Indian Plate from the south-west. On the other hand, underneath the crust vertical stresses arising from for example, the effect of gravitational segregation, thermal expansion and so forth, exert vertical forces on the crust. The mutual action of these two kinds of stresses is thought to determine the seismic activity of the...

The work of certain previous authors indicates that in the crust of China, intensive horizontal stresses exist as a result of the compression from the east by the Pacific Plate and by the Indian Plate from the south-west. On the other hand, underneath the crust vertical stresses arising from for example, the effect of gravitational segregation, thermal expansion and so forth, exert vertical forces on the crust. The mutual action of these two kinds of stresses is thought to determine the seismic activity of the country. This paper attempts to discuss the development of some of the earthquake sources occurred in China. It must b pointd out, many of the viewpoints mentioned here are of course tentative and purely conjectural. The authors welcome criticisms and comments.

根据某些作者的研究,我国境内的地壳承受着来自印度板块和太平洋板块的挤压。因之我国大范围地壳内存在着强大的水平应力场。但另一方面地壳下方上地幔中物质的重力分异和热膨胀等也给上覆地壳施加垂直向的力。这两种力在地壳中的相互作用,共同决定着我国地壳内的地震活动性。本文拟从这个观点讨论大地震的孕育和发生以及某些地震预报问题。但所述的很多论点尚属初步探讨,极不成熟,希望引起学术争论。

The barometry is an important part of studies of magmatic inclusions. Based on authorl's study results, this paper presents and reviews divers barometry methods on magmatic inclusions. There are two barometry methods of magmatic inclusions: direct and indirect. 1.Direct methods Natural basic magmas are often saturated or supersaturated by CO_2. The minerals of basic magmatic rocks and of lherzolite nodules in the alkaline basalts contain fre- quently the primary CO_2 inclusions associated with magmatic inclusions...

The barometry is an important part of studies of magmatic inclusions. Based on authorl's study results, this paper presents and reviews divers barometry methods on magmatic inclusions. There are two barometry methods of magmatic inclusions: direct and indirect. 1.Direct methods Natural basic magmas are often saturated or supersaturated by CO_2. The minerals of basic magmatic rocks and of lherzolite nodules in the alkaline basalts contain fre- quently the primary CO_2 inclusions associated with magmatic inclusions and the primary CO_2-bearing magmatic inclusions. These two sorts of inclusions can be used directly for barometry studies of magmatic inclusions. Natural intermediate-acid magmas contain a lot of dissolved volatie components (mainly H_2O). The magmatic inclusions and the aqueous inclusions coexisting in the minerals of this type of intermediate-acid igneous rocks can be also used directly for barometry studies of magmatic inclusions. 2.Indirect methods In the case of the absence of CO_2-bearing magmatic inclusions or coexisting ma- gmatic inclusions and fluid inclusions(CO_2 inclusions and aqueous inclsuions), we can plot the values of homogenization temperature of magmatic inclusions and their chemical comp osition into some experimental facies diagrams of silicate system, and evaluate the pressures at trapping of magmatic inclusions. Besides this, we can utilise some geothermobarometer for evaluating the pressures at trapping of magmatic inc- lusions in terms of the data of thermometry and chemical composition of magmatic inclusio ns.

测压是岩浆包裹体研究的一个重要方面。本文根据作者的研究结果,介绍和评述岩浆包裹体的各种测压方法,并重点介绍岩浆包裹体测压的直接法和间接法。 1.直接法:天然基性岩浆常饱和或过饱和CO_2。基性岩浆岩和碱性玄武岩二辉橄榄岩包体的矿物常含有与岩浆包裹体共生的原生CO_2包裹体以及原生含CO_2岩浆包裹体。这两种包裹体均能直接用于岩浆包裹体测压研究。天然中-酸性岩浆含大量溶解的挥发组分(主要是H_2O)。这类中-酸性火成岩矿物中共存的岩浆包裹体和含水包裹体也可直接用于岩浆包裹体测压研究。 2.间接法:在缺乏含CO_2岩浆包裹体或共存的岩浆包裹体和流体包裹体(CO_2包裹体和含水包裹体)时,可将岩浆包裹体的均一温度值及其化学成分投于某些硅酸盐系统实验相图之中,估算岩浆包裹体捕获时的压力。也可根据岩浆包裹体的测温和化学成分数据,利用某些地质温度压力计来估算岩浆包裹体捕获时的压力。

The author has studied the trace elements in sphalerite and pyrite from 27 Pb-Zn-pyrite ore deposits of Southern Hunan, and concludes that the value of Ga/In<1 and Co/Ni>1 in sphalerite and pyrite respectively have demonstrated the ore deposits heing hydrothermal type formed during the stage of post-magma acti-vity; and to the contrary, the ore deposits are classified as the sedimentation-trans-formation type. And according to the nature of the elements itself, the author has inquired into the physical-chemical...

The author has studied the trace elements in sphalerite and pyrite from 27 Pb-Zn-pyrite ore deposits of Southern Hunan, and concludes that the value of Ga/In<1 and Co/Ni>1 in sphalerite and pyrite respectively have demonstrated the ore deposits heing hydrothermal type formed during the stage of post-magma acti-vity; and to the contrary, the ore deposits are classified as the sedimentation-trans-formation type. And according to the nature of the elements itself, the author has inquired into the physical-chemical conditions for the formation of the two types of ore deposits as revealed by the correlation value of trace elements men-tioned above; and holds that, in comparison with the hydrothermal ore deposits of the stage of post-magma activity, the sedimentation-transformation type of ore deposits are formed under the conditions characterized by the addition of oxygen that leads the increment, in some degree, of fO_2。

作者研究了湘南27个铅锌黄铁矿床(点)的闪锌矿和黄铁矿的微量元素,得出闪锌矿的Ga/In<1,黄铁矿的Co/Ni>1是岩浆期后热液矿床;反之则是沉积改造矿床。又根据元素本身的性质,对上述微量元素比值差异所反映的两类矿床形成的物理化学条件进行了探讨,认为与岩浆期后热液矿床相较,沉积改造矿床是在有外来氧的加入,致使fO_2有所增高的条件下形成的。

 
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