新疆大学研究生学位论文及论文摘要的书写格式

一、学位论文及论文摘要书写的一般格式

1． 硕士学位论文或博士学位论文，一般应包括下述几部分：

（1）题目：应能概括整个论文最重要的内容。力求简明、恰当、醒目，一般不宜超过20个字。

（2）中文摘要：论文第一页为内容摘要，由题头、摘要正文、关键词等部分组成。正文字数应在300-400字，关键词3-5个。正文应说明本论文的研究目的、方法、成果和结论，要突出本论文的创造性成果或新见解，语言力求精炼、准确。

（3）英文摘要：论文第二页为英文摘要，英文摘要与中文摘要的内容和格式必须一致。中文“摘要”的英文译名统一为“Abstract”。最下方一行为关键词“Key words”(3-5个)。

（4）目录：既是论文的提纲，也是论文组成部分的小标题。

（5）引言(或序言)：内容为：本研究领域的国内外现状，本论文所要解决的问题，该研究工作在经济建设、科技进步和社会发展等某方面的使用价值与理论意义。

（6）正文：是学位论文的主体。(写作方式也可根据学科专业实际情况制定)

如： 一、×××× （居中书写）

（一）××××

1、××××

（1）××××

（7）结论：论文结论要求明确、精炼、完整、准确，认真阐述自己创造性成果或新见解在本领域的意义。（应严格区分本人的研究成果与导师或其他人的科研成果的界限）

（8）注释：硕士论文采用尾注，博士论文采用章后注释。

（9）参考文献：按学位论文中所引用文献的顺序，列于文末。

学术著作：

[序号] 著者.书名[M].版本（初版不写）.翻译者.出版地：出版者，出版年.起止页码. 学术期刊：

[序号] 著者.篇名[J].刊名（外文刊名可按标准缩写并省略缩写点）.出版年，卷号（期号）：起止页码.

论 文 集：

[序号] 著者.篇名.主编.论文集名[C].出版地：出版者，出版年.起止页码.

科技报告：

[序号] 著者.题名[R].报告题名，编号.出版地：出版者，出版年.起止页码.

学位论文：

[序号] 著者.题名[D].保存地点：保存单位，授予年.

专利文献：

[序号] 专利申请者.题名[P].国别.专利文献种类，专利号.出版日期.

技术标准：

[序号] 起草责任者.标准代号 标准顺序号-发布年 标准名称[S].出版地.出版者，出版年. 报纸文献：

[序号] 著者.文献题名[N].报纸名.出版日期（版面次序）.

电子文献：

[序号] 著者.文献题名.电子文献类型标示/载体类型标示.文献网址或出处，更新引用日期.

（10）附录：包括放在正文内过分冗长的公式推导、以备他人阅读方便所需的辅助性数学工具、重复性的数据图表、论文使用的符号意义、单位缩写、程序全文及有关说明等。

（11）在读期间发表论文清单。格式与参考文献格式相同。

（12）致谢。

（13）学位论文独创性声明、学位论文知识产权权属声明。

学位论文制作完毕后，学位申请人及其导师均须签署“学位论文独创性声明”和“学位论文知识产权权属声明”。

“学位论文独创性声明”和“学位论文知识产权权属声明”标准文本如下：

学位论文独创性声明

本人声明，所呈交的学位论文系本人在导师指导下独立完成的研究成果。文中依法引用他人的成果，均已做出明确标注或得到许可。论文内容未包含法律意义上已属于他人的任何形式的研究成果，也不包含本人已用于其他学位申请的论文或成果。与我一同工作的同志对本研究所做的任何贡献均已在论文中作了明确的说明并表示谢意。

本人如违反上述声明，愿意承担由此引发的一切责任和后果。

论文作者签名： 日期： 年 月 日

学位论文知识产权权属声明

本人的学位论文是在学期间在导师指导下完成的，知识产权归属学校。学校享有以任何方式发表、复制、公开阅览、借阅以及申请专利等权利。本人离校后发表或使用学位论文或与该论文直接相关的学术论文或成果时，署名单位仍然为新疆大学。

本学位论文属于：

保密 □，在 年解密后适用于本声明。

不保密□。

（请在以上方框内打“√” ）

论文作者签名： 日期： 年 月 日

导师签名： 日期： 年 月 日

2．论文摘要(另行撰写)

论文摘要是原文的浓缩，要论点清晰，并能集中地反映论文的精华。有新见解(指在前人的基础上的进展)、新观点、新资料、新的研究方法和主要结论。摘要要中、英文各一份，硕士学位论文摘要应以1000～1500字为宜，博士学位论文摘要应以1500～2000字为宜。

二、学位论文及论文摘要的规格

1．博士、硕士研究生学位论文及论文摘要一般使用标准简化汉字，排版采取紧凑格式，不允许留有大量空白。要求字迹和标点符号清楚、工整、正确。论文纸张为A4纸（210×297mm）标准格式，版芯尺寸为160×237mm。博士论文要求双面打印，硕士论文根据实际情况可单、双面打印。

2．中文摘要及正文用宋体小四号字，英文摘要用Times New Roman体小四号字，行距为25磅，字间距为标准。参考文献、注释、附录等用宋体五号字。页码从引言开始按阿拉伯数字连续编排，页码位于页面底端，居中书写。论文中图表、附注、参考文献、公式一律采用阿拉伯数字连续(或分章)编号。图序及图名置于图的下方；表序及表名置于表的上方；论文中的公式编号，用括弧括起写在右边行末，其间不加虚线。图表中如用5号字有困难，可小于5号字，但不得小于7号字。

三、学位论文及论文摘要的装订要求

学位论文的封面均采用全校统一格式，全日制博士学位论文的封面为红色布纹纸，全日制硕士学位论文封面为白色铜版纸，同等学力在职申请硕士学位论文、专业学位论文、高校教师在职攻读硕士学位论文封面为深蓝色布纹纸。学位论文一律在左侧装订，要求装订、剪切整齐，便于使用。摘要的装订要求与论文相同。各学院可统一在学校印刷厂印制、装订。

四、论文和论文摘要的印制份数

1．博士学位论文，应按照导师、学术评阅人、答辩委员会成员每人一本、报送研究生院6本和本学院留存的册数，及有关人员的要求，确定打印或复印的册数，一般应有22本。

2．硕士学位论文，应按照导师、学术评阅人、答辩委员会成员每人一本，报送研究生院5本和学院留存的册数，及其它有关人员的要求，确定打印或复印的册数，一般应有12-17本。

3．博士论文摘要送研究生院25份，硕士论文摘要送研究生院5份。

四、同等学力申请硕士学位、专业学位、高校教师在职攻读硕士学位人员适用本规定。

 

第二篇：新疆大学研究生课程考试(查)论文封面格式

新疆大学研究生课程 2014 ——2015 学年 第 二 学期 《 专业英语 》 课程名称： 专业英语 任课教师：学 院： 资源与环境科学学院 专 业： 生态学 学 号： 姓 名：

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Summery

The first part is how to read maps, A map is a representation of a geographic area, usually a portion of the earth’s surface. It may be shown in many different ways, from a traditional map printed on paper to a digital map built pixel by pixel on the screen of a computer. Maps can show almost anything, from the electric supply grid of your community to the terrain of the Himalayas to the depths of the ocean floor. People make maps from data they collect with certain tools. The world is constantly changing both physically and culturally, so maps can become outdated, no longer showing the world accurately. Maps are biased. Because maps generally do not show every single feature of a chosen geographic area—every tree, house, and road—the cartographer must decide the projection and scale for the map and decide how much detail to present. Map has few types, such as roads, borders, vegetation, or statistical data. Maps can be divided by theme into three categories. Maps are made in many different forms. Computer maps are the most versatile. A mapping program can dynamically show many different views of the same subject, allow changes in scale, and incorporate animation, pictures, sound, and Internet links to sources of supplementary information. Map Elements include Projection, Legend.The surface of the earth is curved and maps are flat, whether they’re printed maps or computer screen pictures. This means that all maps except for globes and pictures of globes are distortions of how the earth really looks. Some maps have other special-purpose coordinate systems, such as the State Plane Coordinate System used on maps in the United States or the Universal Trans-Mercator (UTM) system used on many military maps. Maps use sets of symbols to indicate the placement of real objects. The legend is a block of text or a window in which the symbols used on the map are explained.

The Second part is Geomorphology, in this part; it introduces the content of geomorphology’s study, historical geomorphology, process geomorphology, under lying dynamics, weathering and erosion.

The Third part is Glaciation, Glacier, an enduring accumulation of ice, snow, water, rock, and sediment that moves under the influence of gravity. Glaciers form where the temperature is low enough to allow falling snow to accumulate and slowly transform into ice.The types of glaciers include Ice Sheets, Ice Caps, and Ice Fields; Valley, Alpine, and Piedmont Glaciers, Rock Glaciers. The glacial formation and movement include Transformation of Snow to Ice; The Anatomy of a Glacier;and Glacier Movement.The effects of glaciets on land include Glacial Erosion, Glacial Deposits,The glaciers and climate change Glaciers are very sensitive to climate change. Their size, life span, and history of growth and retreat all depend strongly on climate conditions. And Historical climate records generally do not go back more than 2,000 years, but past climates can be reconstructed from many different sources of evidence.

The Fourth part is Monsoons, tropical storms and tornadoes. Colliding cold and warm air masses create storms, resulting in high winds and heavy rains. The violence or duration of these storms can lead to extensive property damage and loss of life. The world’s most significant and disastrous climatic events are monsoons, tropical storms, and tornadoes. Monsoons, The monsoons are seasonal winds that bring torrential rains in the summer and sunny and dry weather in the winter. These winds blow in response to temperature differences between air over the land and air over the sea. Tropical

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storms are large rotating storm systems that form in the Atlantic, Indian, and Pacific

oceans. Hurricanes and typhoons form during the hottest months of the year as

moisture evaporates from warm oceans in the calm doldrums near the Equator. And

can be very damaging to low-lying coastal areas, causing widespread destruction from

surging seas, flooded rivers, and high winds. Tornadoes, although short-lived, are the

most violent storms on the planet.

The Fifth part is Mountains, this part include formation of mountains, uplift, volcanoes, erosion, elevation, humans and mountains. the highest mountain system in the world. During the Paleozoic and Mesozoic eras—570 million to 65 million years ago—the rocks that form the Himalayas were

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being laid down as sediment on the floor of an ancient sea. A collision between plates triggers deformation and thickening of the crust, which in turn leads to crustal uplift and mountain formation.

A common process produced by horizontal compression is the deformation of layers into folds or wrinkles. Mountains formed by volcanic activity are well known because of their usually isolated occurrence and the danger they pose. Mountains are usually very temporary features in terms of geologic time. Many forces are constantly at work to erode them. Air, water, and ice cause the physical and chemical breakdown of mountain rocks that are exposed to the elements. Rain erodes weakened rock exposures, and streams carve deep gullies and ravines in mountainsides, mainly during flooding. The elevation of a mountain peak is the height of the summit above sea level. Yet the appearance of mountains can be deceiving. Some high mountains nestle among other high peaks, and their summits do not appear to be much higher than the surrounding topography. Mountains affect life in many ways. Apart from their obvious mineral, forest, agricultural, and recreational resource value, they exert a significant influence on climates and help determine the course of economic and historical trends.

The Sixth part is Seasons: Climate, Stars, and Earth Changes. This has two parts. One is it introduce the drama of the seasons, another is tell the cause of seasons. The reason of drama are day length, solstices and equinoxes, the tropics, star positions, climate, physical effects of seasonal climate, ocean currents, animal migration, temperature, moisture, air pressure, winds and currents storms, floods, droughts, and global warming.

The Seventh part is the hydrologic cycle. The hydrologic cycle is what is known as a closed system because there are no external inputs or outputs of water to or from the system. The same water has been continually circulating since the beginnings of life on Earth. The other main long-term storage mechanisms are aquifers. The Cycle :The Sun's heat drives the hydrologic cycle. As wind blows across the surface of the ocean, this heat causes water to evaporate from the sea and become absorbed into the air as water vapor—the amount absorbed depends on the temperature of the water. The water vapor in the atmosphere forms clouds.

The Eighth part is tides and waves. Include tidal energy, waves and tides. Mainly introduce these formation and use.

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