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地质外文文献翻译中英文对照

地质外文文献翻译中英文对照
地质外文文献翻译中英文对照

地质外文文献翻译中英文对照

长安大学资源学院英语文献翻译

学院地球科学与资源学院

专业资源勘查工程

学生姓名_____________

学号201127020308 ____________

指导教师张亚敏_____________________

2015年6月18日

Title:Orthomagmatic ore deposits

On e.Orthomagmatic ore deposits

The magma contains a certain number of metal and volatile components of the silicate melt. All kinds of magma after crystallizatio n and differe ntiatio n, make the formi ng materials dispersed in the magma gathered and formed deposits.And this deposits is called magmatic deposits.

Magmatic deposits formed in the magmatic stage, the source of the material of the deposit is the main ore-bearing magma.

Magmatic deposits is the product of the magma by crystallizatio n and differe ntiatio n, and gen erally have the followi ng properties:

1、Deposits have the mainly relationship with the mafic and ultramafic rocks.A nd a small nu mber of magmatic deposits with alkaline rocks or magmatic carbonatite-related.

Mineralization and diagenesis often begin at the sametime.And this is typical of syngenetic ore deposits. Few mineralization of the magmatic deposits may be continued to a later time, but generally does not exceed

a total period of magmatic activity.

2、The magmatic deposits ore body majority present stratiform, lenticular and podiform and so on.And they produced in the magmabody,and the wall rock of containing ore is the mother rock.Few cases,orebody presenting vein and stockwork enter the wall rock which outside of the mother rock Between the ore body and the wall rock generally is gradual change or rapid gradual change relationship.Only penetration magmatic deposits have the clear boundaries with the wall rock.

3、Except the rare and rare earth elements deposits of the magmatic carbonatite due to special causes have some alteration about the wall rock,the vast majority of magmatic deposits surrounding rock does not have a significant alteration phenomenon.

4、The ore and the wall rock basically have the same mineral composition, whenthe useful minerals of the rock body aggregate and reach a certain size,they become the orebody.

5、The ore of magmatic deposits often

have,disseminated,the banded,eye porphyritic,dense massive,brecciated and so on,ore structure.The ores structure can be broadly divided into the

following categories: I.Structure sub-the different magmatic condensate crystalline or stacking interactions; II.Reflect the structure of the immiscible fluid crystallization process III.Reflect the changes in the structure of the physical and chemical conditions.IV.Epigenetic structure.

6、The magmatic deposits forming temperature is high, generally between 1200 to 700 ° C. The mineralization depth changes,generally formed in the ground a few kilometers to tens of kilometers.

Tow.The formation conditions of magmatic deposits

Magma deposits are mainly derived from the magma, it is the combined effects of the product by a variety of geological factors, which playing a leading role is the geochemistry of ore-forming elements traits, the magmatic rock conditions, tectonic conditions and physical and chemical conditions and so on.

1、Control the conditions of magmatic rocks formed by magmatic deposits

Magma is the main provider of the metallogenic material

of the magmatic deposits and the medium of containing mineral medium.Therefore,how much of the content of useful components of magma is the possibility of the formation of magmatic deposits.

I. Magmatic rocks metallogenic specialization

Metallogenic specialization of magmatic rocks in the genesis of

magmatic rocks with endogenous deposits showed regular contact, and specific types of magmatic rocks are often produced specific types of deposits.

a)With mafic and ultramafic intrusive rocks related deposits

Mafic and ultramafic rock is the complex igneous complex formed by the combination of a variety of rock types, rock types from a single rock composedof rock massis relatively rare.The size of the rock mass ranging mostly small,and rock strains, rock cover, rock, bedrock is the most common form of the rock mass. With facies and the different combinations,the mafic and ultramafic rocks can be divided into three types.

b)Mineral deposits associated with syenite, nepheline

syenite and carbonate igneous complex

Relating to magmatic deposits of these rocks are mostly produced with the form of rock strain,the different components of rock mass facies zone often has ring distribution.

II. The role of the volatile components in the magma

The magma volatile components have the low melting point,highly volatile and they can delay the condensation rate of the magma, make the magma have more fully differentiation.

III. Magmatic assimilation have an influence on the mineralization of the magma Deposits

IV. Beyond one period of magma intrusion on control of the mineralization

2、Tectonic conditions that control the formation of magmatic deposits

Tectonics have a major impact on the type of magmatic deposits, distribution, the most magmatic deposits associated with mafic and ultramafic igneous rocks on the Causes and space. Mafic and ultramafic magmaformed by partial melting of mantle material,so the deep fault cuts through the crust to reach the upper mantle have a strict control effect on the mafic, ultramafic rocks and magmatic deposits which have some relationship with them.

Three.Magmatic deposits formation and its characteristics

1、The process of the magm'a s useful components analysis, aggregation and positioning is called magmatic mineralization.

Because the magmatic deposits mafic - ultramafic petrogenesis process is very complex, the mineralization also is varied.According to the way and feature of the mineralization,magmatic mineralization can be divided into four categories,the crystallization differentiation mineralization, melting away from the mineralization the magma eruption mineralization and magma eruption mineralization.

When magma is condensed, with the temperature gradually decreased, the various mineral sequentially from which crystallized out,

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韶关学院 期末考核报告 科目:专业英语 学生姓名: 学号: 同组人: 院系: 专业班级: 考核时间:2012年10月9日—2012年11月1 日评阅教师: 评分:

第1章英文阅读材料翻译 (1) 第2章中文摘要翻译英文 (3) 第3章中文简历和英文简历 (4) 第4章课程学习体会和建议 (6) 参考文献 (7)

第1章英文阅读材料翻译 Mechanization and Automation Processes of mechanization have been developing and becoming more complex ever since the beginning of the Industrial Revolution at the end of the 18th century. The current developments of automatic processes are, however, different from the old ones. The “automation” of the 20th century is distinct from the mechanization of the 18th and 19th centuries inasmuch as mechanization was applied to individual operations, wherea s “automation” is concerned with the operation and control of a complete producing unit. And in many, though not all, instances the element of control is so great that whereas mechanization displaces muscle, “automation”displaces brain as well. The distinction between the mechanization of the past and what is happening now is, however, not a sharp one. At one extreme we have the electronic computer with its quite remarkable capacity for discrimination and control, while at the other end of the scale are “ transfer machines” , as they are now called, which may be as simple as a conveyor belt to another. An automatic mechanism is one which has a capacity for self-regulation; that is, it can regulate or control the system or process without the need for constant human attention or adjustment. Now people often talk about “feedback” as begin an essential factor of the new industrial techniques, upon which is base an automatic self-regulating system and by virtue of which any deviation in the system from desired condition can be detected, measured, reported and corrected. when “feedback” is applied to the process by which a large digital computer runs at the immense speed through a long series of sums, constantly rejecting the answers until it finds one to fit a complex set of facts which have been put to it, it is perhaps different in degree from what we have previously been accustomed to machines. But “feedback”, as such, is a familiar mechanical conception. The old-fashioned steam engine was fitted with a centrifugal governor, two balls on levers spinning round and round an upright shaft. If the steam pressure rose and the engine started to go too fast, the increased speed of the spinning governor caused it to rise up the vertical rod and shut down a valve. This cut off some of the steam and thus the engine brought itself back to its proper speed. The mechanization, which was introduced with the Industrial Revolution, because it was limited to individual processes, required the employment of human labor to control each machine as well as to load and unload materials and transfer them from one place to another. Only in a few instances were processes automatically linked together and was production organized as a continuous flow. In general, however, although modern industry has been highly mechanized ever since the 1920s, the mechanized parts have not as a rule been linked together. Electric-light bulbs, bottles and the components of innumerable mass-produced

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