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2007年全国第七次高等学校毕业生就业研究优秀论文获奖...

2007年全国第七次高等学校毕业生就业研究优秀论文获奖名单（计算机随机排名）论文名称作者姓名工作单位等级高校毕业生创业孵化基地建设研究刘铸辽宁省高等学校毕业生就业指导服务中 1 理工科重点大学毕业生职业期望与实际就业状况研究杨克旭、梁茵大连理工大学1提高高职院校毕业生就业能力的对策与思考许跃吉林工业职业技术学院招生就业指导处1高校毕业生到民营企业就业问题调查与研究田一闳云南教育厅学生处 1 高等教育大众化进程中大学生就业工作研究马于强、刘坤井冈山学院招生就业指导处 1 地方农业院校就业指导工作实践与思考游京峰、张高亮、涂雯雯、胡蝶。

江西省高等院校毕业生就业工作办公室 1 对当前高校毕业生创业与创业教育活动的调查分析与研究鲍勇、尚昌庚安徽省就业指导中心1浅析贫困大学生就业问题及对策鲍丽娟、李光彬、夏富生、胡晓浩、彭化慧合肥工业大学 1 当前大学生就业环境分析及促进就业的对策思考林禄明安徽省就业指导中心 1 甘肃省大学生就业意向调查报告魏军、李宏伟兰州交通大学 1 少数民族大学毕业生就业问题研究王扎西、钟福祖、刘燕华、董化琪、马莉。

西北民族大学1独立学院学生就业的现状和对策齐晓琴兰州商学院陇桥学院1改革高等教育体制，促进大学生就业陈建恩兰州大学 1 元认知训练在大学生职业辅导中的应用孙立国兰州大学1大学城就业指导资源共享探索侯永雄华南师范大学1大学生职业生涯规划第一课模式探讨李向明广东技术师范学院 1 运用政策导向促进高校毕业生向民营企业流动沈鸿银广西高校毕业生就业指导中心 1 普通高校残疾毕业生就业问题的观念障碍与政策缺失金海燕、谢红梅浙江大学1基于职业生涯理论的大学生就业指导体系的探索王慧、刘青、李澎林浙江工业大学 1 高职毕业生就业与区域经济社会发展芦京昌杭州职业技术学院 1 地矿人才就业状况分析侯建湘、周春燕中国地质大学（武汉）11关于提高高校毕业生就业质量的思考方伟北京大学 1 高校毕业生就业诚信问题分析及解决途径初探欧阳沁、祁金利、陈旭清华大学1强化教育，创新思路，大力向国防科技工业基层输送优秀人才程基伟北京航空航天大学1高校开展创业教育体制的初探易宏琤、程武、路英海、张闯。

初审结果

第七屆小論文寫作比賽初審結果（以領域排序）
第七屆小論文寫作比賽初審結果第1頁共6頁
第七屆小論文寫作比賽初審結果第2頁共6頁
第七屆小論文寫作比賽初審結果第3頁共6頁
第七屆小論文寫作比賽初審結果第4頁共6頁
第七屆小論文寫作比賽初審結果第5頁共6頁
初審結果之備註：
1.初審結果之「過」：進決賽；「未過」：不能進決賽。

2.進決賽比率：生活5/5=100.0%。

自然15/16＝9
3.8%。

社會18/21＝85.7%。

英文2/6=33.3%。

國文0/1=0%。

藝術2/2=100.0％。

3.進決賽（通過）之總比率42/51=82.4%（上屆80.8%）。

未進決賽總比率9/51=17.6（上屆19.2%）。

第七屆小論文寫作比賽初審結果第6頁共6頁。

嵌入式WEB服务器网关系统的研究与实现

大连理工大学硕士学位论文
保证系统的安全性,防止非授权用户访问嵌入式系统。连接菜单让用户选择是网关和WEB服务器功能。连接菜单包括UDP连接和TCP连接子菜单。UDP连接用于网关传输,只需输入嵌入式系统的口地址,就可以收发UDP数据包,嵌入式系统收到UDP 数据包后直接封装成CAN协议数据包,发送到相应地址的智能设备DYZB.101B上,同时将DYZB.101B上传的CAN协议数据包封装成uDP数据包返回给客户端。TCP连接用于WEB服务器传输,输入嵌入式系统的口地址,点击建立连接按钮,然后等待,直到嵌入式WEB服务器发送连接已建立信息。此时,客户端和嵌入式WEB服务器已经建立了TCP连接,沿着这个连接就可以收发TCP数据包。查询菜单中定义了监控系统中所有的查询信息,在相应的查询信息菜单上点击一下,监控软件就自动发送该查询信息的HTTP请求报文,接收到}盯rP应答报文后将网页显示在文档中。设置菜单中定义了监控系统中所有的设置信息,在相应的设置信息子菜单上点击一下,就会弹出相应的设置界面,用户填好信息后点击发送按钮,监控软件就自动发送设置参数的HTTP请求报文,等待DYZB.101B的设置成功信息的回复。收到回复后,上传给监控软件,就在文档中显示设置成功的网页。
如图4.4所示。Iris软件捕获数据包窗口主要分为三个部分。最左边显示数据包各层协议的信息,称作协议分析栏。右边分为上下两部分,右上部分显示捕获的数据包,称作收发数据包栏;右下部分显示解码数据包的ASCII代码,称作解析数据包栏。在收发数据包栏中,数据包按收/发时间排序,并依次显示每个数据包的收/发时间、源MAC 地址、目的MAC地址、数据包协议类型、源m地址、目的m地址、源端口、且的端口和数据长度等信息。在协议分析栏,根据OSI七层模型,将数据包分解成若干部分。每一个数据包的报头(MAC、IP、ICMP、TCP和U】)P)将会在这里显示出来。解析数据包栏和他们相互关连,在收发数据包栏上,用鼠标单击任一个数据包,解析数据包栏就显示该数据包的解码,协议分析栏就显示该数据包的各层协议报文,并解析报头。在协议分析栏中点击数据包的任一部分,解析数据包栏中就会高亮度显示该部分的ASCII。

王陈电磁波在脉冲星磁层中的传播-国家天文台

充满相对论流动的等离子体（开放磁力线区域）

电子－正电子对等离子体：Np ~ Ne （有一点不同）电子和正电子都沿磁力线方向流动 Lorentz 因子: γ~ 10 -106 , γp ~ γe （可能有一点不同）等离子体密度: η= N / N_GJ = 1 – 105. 不能确定。

辐射初始状态
射电辐射，rem ~ 10’s-100’s RNS . （曲率辐射，ICS） X-ray，来自星体表面（如polar Ω cap），热辐射 μ 初始线偏振 α

O模：
k
ζ B
E // k-B plane X模： E ⊥ k-B plane
几种典型的传播效应
波模耦合（wave
Weinberg et al. 2003
Weinberg et al. 1999
Magnetic-Pole Model for Emission Beam
• Emission beamed tangential to open field lines • Radiation polarised with position angle determined by projected direction of magnetic field in (or near) emission region (Rotating Vector Model)
Mean pulse shapes and polarisation
P.A. Stokes I Linear
Stokes V
Lyne & Manchester (1988)
Orthogonal-mode emission – PSR B2020+28

2007年第2卷中文总目次

山苍子油对小鼠系统性新生隐球菌感染的实验研究 …………………… 万力李伟王永强等（３２）中国大陆马尔尼菲青霉病的临床表现及流行病学特征的系统评价 … … 赵国庆冉玉平向耘（８６）
利用蛋白质组学技术筛选隐球菌作用血管内皮细胞后差异表达蛋白
王强李铁男（４）１６
我国首例肌曲霉病及其试验研究
…… …… …… …… …… …… … 李东明
…… …… …… …… … 农东晓
修典荣
李菊裳朱敬先
艾滋病合并咽喉马尔尼菲青霉菌病的研究
林生地霉所致小鼠系统感染的形态学研究 …… …… …… …… … 尹瑞瑞
土曲霉致双外耳道曲霉病 … …… …… …… …… …… …… …… … 李发增
冉玉平
代亚玲等（２）１９
对多烯类药物耐药的１株黄曲霉临床株耐药性的初步研究 …………… 刘伟万结陈伟等（３）１３
两性霉素Ｂ和伏立康唑对临床真菌的体外抗菌活性分析 … …… 窦红涛北京朝阳医院深部真菌感染的临床分析和药敏试验徐英春杨启文等（３）１７杜小玲等（４）１０徐红等（４）１３李若瑜等（９）１３
… … … … … … … … … … … … … … … … … … … … … … … … … … … … … … … …
徐楠
邹豪
温海等（ＯＩ）沈柱（４１）温海等（０２）张明昱等（７１）
甲真菌病多点平皿培养法与常规试管培养法的比较 …… …… …… …… …… …… … 刘斌威海地区５７例甲真菌病真菌培养结果分析 … …… …… …… … … 岳喜昂刘卫兵４束状刺盘孢的体外培养条件研究 … …… …… ……… … ……… … …… … 杨连娟徐红

2007级毕业设计(论文)表格

封面潇湘职业学院
学生毕业设计（论文）
题目：压线板冷冲模设计
系部：
专业：
学号：
姓名：
指导老师：
开题时间：
完成时间：
潇湘职业学院教务处制
潇湘职业学院
毕业设计（论文）课题学生选题表
潇湘职业学院教务处制
毕业论文册内内容1
潇湘职业学院
毕业设计(论文)任务书
系部:_机械工程__ 指导教师:___鲁铁山__
专业:_模具设计与制造班级:_________
学号:__________ 姓名:__________ 日期: 2010 年2月28日
潇湘职业学院教务处印制
毕业论文册内内容2
本表一份，由学生选题后指导教师填写发送给学生开题
潇湘职业学院
毕业设计（论文）鉴定登记表
系专业
级班
课题名称：
学号：
姓名：
指导教师：
年月日
毕业论文册内内容3
填写表说明
一、毕业设计（论文）简况，由学生本人填写。

内容包括毕业设计（论文）内容摘要及做毕业设计（论文）的收获体会及存在的问题。

二、毕业设计（论文）成绩评定，按优秀、良好、及格、不及格四级评分制记分。

三、填写时一律用黑、蓝墨水笔，字迹清楚，内容简明扼要。

四、本表一式两份。

一份随毕业设计装订，一份入学籍档案。

潇湘职业学院毕业设计（论文）封底。

一种解析Word文件信息的方法及其系统[发明专利]

(10)申请公布号 CN 101980183 A(43)申请公布日 2011.02.23C N 101980183 A*CN101980183A*(21)申请号 201010285333.5(22)申请日 2010.09.17G06F 17/21(2006.01)(71)申请人深圳市万兴软件有限公司地址518057 广东省深圳市南山区高新南一道TCL 大厦A 座901(72)发明人解辉(74)专利代理机构深圳市君胜知识产权代理事务所 44268代理人刘文求韩金明(54)发明名称一种解析Word 文件信息的方法及其系统(57)摘要本发明公开了一种解析Word 文件信息的方法及其系统，该方法包括：将待解析的Word 文件转换为Word_XML2003格式文档的中间文件；解析Word_XML2003格式文档中元素的基本信息，并将解析得到的信息按照Word 的规则进行组合；将解析组合后的对象写入XML 文件。

由于采用了Word_XML2003格式文档作为中间文件，并在解析Word_XML2003格式文档后按照Word 的规则进行组合，不仅在解析比较复杂的元素时不会造成属性丢失，而且还避免了频繁的调用Com 接口，节约了系统资源，高效稳定地解析了所有格式的Word文件信息，特别适合满足需要批量解析各种版本的Word 文件信息的情况下使用。

(51)Int.Cl.(19)中华人民共和国国家知识产权局(12)发明专利申请权利要求书 2 页说明书 6 页附图 3 页1.一种解析Word文件信息的方法，其特征在于，包括以下步骤：将待解析的Word文件转换为Word_XML2003格式文档的中间文件；解析Word_XML2003格式文档中元素的基本信息，并将解析得到的信息按照Word的规则进行组合；将解析组合后的对象写入XML文件。

2.根据权利要求1所述的解析Word文件信息的方法，其特征在于，在转换为Word_ XML2003格式文档的步骤中，具体包括以下步骤：初始化Word对象；通过Word实例对象创建一个Word文档对象；将Word对象设置为后台运行；使用文档对象导入一个Word文件；将Word格式文档另存为XML2003格式文档。

2007年1～4期总目次

・
试验与研究・
一
高超声速推进系统用单膨胀斜面喷管型面设计和流场模拟 …… ……… … 王占学。刘爱华。元虎蔡发动机起动过程部件特性的一种改进描述 … ………… …… …… ……… … 刘建勋，李应红，张东方大转角压气机静子叶栅附面层吹吸数值研究 ……… ……… …… …… ………… …… 邓昌清。胡骏
高温升火焰筒壁面及头部复合冷却设计分析 …… ……… ……… …一 ……… …… …・李彬，程波（－８３）危险部位数目对轮盘低循环疲劳寿命的影响研究 … …… ……… …… …… 王卫国，卿
ＦＩ６粉末高温合金亚尺寸轮盘研制及试验验证Ｇ－［９
利用楔形突体结构改善气膜冷却效率的数值研究 ……… ……… …… ……… …… … 杨成凤，张靖周（－２２３）狭长出口弯曲混合管一体化红外抑制器红外特性分析 … …… ……… ……… …… … 唐正府，张靖周（－７２３）旋转状态下篦齿流量特性试验研究 …… …… ……… ……… …… ……… … 王代军．苏云亮，罗翔（１２）高转速对直通型篦齿封严特性影响的试验研究 ……… …… …… ……… ……… ……… …… ………
… … … … … … … … … … … … … … … … … … … … … …
… ……… …… ……… ……… …… ……… ………
…
曹凤兰。卿华，古远兴，吴长波，周全（－５３１）
基于低雷诺数条件的风扇／压级气动设计增

Fang XM etal2007

High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonicuplift of the NE Tibetan PlateauXiaomin Fang a,b,⁎,Weilin Zhang a ,Qingquan Meng b ,Junping Gao b ,Xiaoming Wang c ,John King d ,Chunhui Song b ,Shuang Dai b ,Yunfa Miao baCenter for Basin Resource and Environment,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,P .O.Box 2871,Beilin North Str.18,Beijing 100085,ChinabKey Laboratory of Western China's Environmental Systems,Ministry of Education of China &College of Resources and Environment,Lanzhou University,Gansu 730000,ChinacDepartment of Vertebrate Paleontology,Natural History Museum of Los Angeles County,900Exposition Boulevard,Los Angeles,CA 90007,USAdGraduate School of Oceanography,University of Rhode Island,URI Bay Campus Box 52,South Ferry Road,Narragansett,RI 02882-1197,USAReceived 31December 2006;received in revised form 23March 2007;accepted 23March 2007Editor:R.D.van der HilstAvailable online 31March 2007AbstractThe closed inland Qaidam Basin in the NE Tibetan Plateau contains possibly the world's thickest (∼12,000m)continuous sequence of Cenozoic fluviolacustrine sedimentary rocks.This sequence contains considerable information on the history of Tibetan uplift and associated climatic change.However,work within Qaidam Basin has been held back by a paucity of precise time constraints on this sequence.Here we report on a detailed paleomagnetic study of the well exposed 4570m Huaitoutala section along the Keluke anticline in the northeastern Qaidam Basin,where three distinct faunas were recovered and identified from the middle Miocene through Pliocene.Constrained by these faunal ages,the observed thirty-three pairs of normal and reversed polarity zones can be readily correlated with chrons 2n-5Br of the GPTS.This study assigns the age of the section to the interval between ca.15.7Ma to 1.8Ma.In addition,the widely used stratigraphic units the Xia Youshashan,Shang Youshashan,the Shizigou and Qigequan Formations were formed at N 15.3Ma,15.3–8.1Ma,8.1–2.5Ma and b 2.5Ma,respectively.We obtained a very high average sedimentation rate of ∼33cm/ka over the entire interval 15.7to 1.8Ma.Furthermore,the average sedimentation rate is punctuated by three intervals of persistent rapid increases starting at about ∼14.7Ma,8.1Ma and 3.6Ma.These intervals are interpreted as times of rapid uplift and fast exhumation of the NE Tibetan Plateau.©2007Published by Elsevier B.V .Keywords:magnetostratigraphy;Neogene;Qaidam Basin;NE TibetanPlateauEarth and Planetary Science Letters 258(2007)293–306/locate/epsl⁎Corresponding author.Center for Basin Resource and Environment,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,P.O.Box 2871,Beilin North Str.18,Beijing 100085,China.Tel.:+861062849697;fax:+861062849886.E-mail address:fangxm@ (X.Fang).0012-821X/$-see front matter ©2007Published by Elsevier B.V .doi:10.1016/j.epsl.2007.03.0421.IntroductionThe Qaidam Basin (∼850km long ×150–300km wide =∼121,000km 2)is the largest basin on the north-eastern Tibetan Plateau.It is bounded by the Qiman Tagh –Kunlun Shan (Mts.)to the south,the Altyn Tagh (Mts.)to the northwest,the Qilian Shan (Mts.)to the northeast and the Ela Shan (Mts.)to the east.It has an average elevation of 3000m above sea level,in contrast to the surrounding mountains with elevations of 4000–5000m (Fig.1).It has been interpreted to have been a closed inland basin since the Paleocene and is filled with a maximum thickness of ∼12,000m of Cenozoic sedi-ments (the thickest known section of Cenozoic continent sediments)shed from the surrounding mountains [1–3].It is located in the arid region of North China,but is still affected by the front of the Asian monsoon.The sedimentary record of this basin attracts considerable attention because:(1)it contains a great potential record of the initiation and development of the Asian monsoon and of Asian aridification [4–6];(2)it provides a record of the ongoing growth of the Tibetan Plateau flat surface through the infilling of basins [7,8];(3)it provides a typical example for Cenozoic crustal detachment [9,10];and (4)it provides a record of the deformation and uplift of the Kunlun Shan and the Qilian Shan,especially the activation of the huge (1500m long)strike –slip Altyn Tagh fault that has been thought to be a key boundary to transfer the deformation caused by the collision of India with Asia by continental extrusion [8,11,12].Several tectonic models predict that either the Qaidam Basin and the northeastern Tibetan Plateau are the most recently deformed and most tectonically active part of Tibet [7,8,10],or comprise the entirety of the Cenozoic deformed block [13].Unfortunately,until our work,we have not had accurate chronology and paleoenviron-mental and tectonic records from the Qaidam Basin to either to reconstruct the histories of the Asian monsoon and Asian desertification,or for testing the tectonic models.This lack of an accurate chronology is largely caused by a previous paucity of mammalian fossils or other means of obtaining geochronology from the thick Cenozoic sedimentary sequences.This barrier was slowly breached by a steady stream of discoveries of fossil mammals in the east Qaidam Basin since 1998[14,15]that followed earlydiscoveriesFig.1.DEM presentation of the geomorphology of the Qaidam Basin and its surrounding mountains.1:Honggouzi anticline;Thrust belt:North Qaidam marginal thrust belt.294X.Fang et al./Earth and Planetary Science Letters 258(2007)293–306by a Swedish paleontologist,Birger Bohlin.With fewexceptions,the mammal sites are located in thenortheastern Qaidam Basin in the vicinity of Delinghaand Huaitoutala and span the stratigraphic interval be-tween the middle Miocene and Pliocene[16,17](Fig.8).We now have sufficient mammal finds that are agediagnostic to provide chronological constraints on anumber of fossiliferous sections.Encouraged by thesefindings,we choose the Huaitoutala section,10km southof the village of Huaitoutala,for detailed paleomagneticstudies,because it bears seven layers of fossil mammalscontaining components of most of the fossil mammalgroups found in the region(Fig.2).A chronology basedon an integrated study of the mammalian fossils andpaleomagnetic polarity reversals obtained from the rel-atively long and continuous section offers the best reso-lution possible for a continental setting that does notcontain volcanic rocks that can be radiometrically dated.The absence of dateable volcanic rocks is typical ofmuch of Asia during the Cenozoic[16].2.Geologic setting and stratigraphyThe high relief contrast between the depressedQaidam Basin and highly uplifted surrounding moun-tains is controlled by the large boundary faults betweenthem[1,2,11,12](Fig.1).The north Kunlun fault,derived from the Kunlun fault belt along the QimanTagh and the Kunlun Shan,bounds the southern marginof the Qaidam Basin.The Kunlun fault runs roughlyeast–west for about1100km and is a major strike–slipfault thought to absorb and transfer deformation im-posed by the collision of India with Asia[11,12](Fig.1).The impressive1500-km long,NE–SW left-lateral strike–slip Altyn Tagh fault cuts through thenorthwestern margin of the Qaidam Basin.Between ∼350–400km[18–20]and∼500–700km displace-ment[21,22]is thought to have taken place along thefault.This displacement has caused not only the depres-sion and deformation of the Qaidam Basin and formationof the Altyn Tagh mountains,but has also transferredmuch of the deformation into the broad region of the NanShan–Qilian Shan,resulting in an intense uplift of theregion[2,8,11–13,23](Fig.1).The northern margin ofthe Qaidam Basin is bounded by the Nan Shan and theZongwulong Shan faults(also called the south marginalfault of Qilian Shan;F1in Figs.2and3)that run in aNWW–SEE direction.These faults are not only geo-metrically but also dynamically linked with the AltynTagh fault to absorb the transferred deformation andhave caused strong deformation and uplift of the NanShan.This transfer has formed a broad thrust belt(ca.440km long×65km wide=30,000km2)in the northernmargin of the Qaidam Basin,called the north Qaidammarginal thrust belt(NQMTB),which parallels thesouthern margin of the Qilian Shan[1,2](Fig.1).Aseries of north-dipping thrusts and their associated south-dipping backthrusts can be clearly observed in the sur-face,satellite and DEM images and seismic profileswithin the NQMTB in the study area.These thrusts andbackthrusts fall roughly into four groups of tectonicunits,the Delingha depression,the Olonbuluk upheaval,the South Olonbuluk depression,and the Emonike up-heaval(Figs.1–3).To the north and south of theNQMTB are the tectonic units of the Qilian Shan and thePlio-Quaternary depocenter of the Qaidam Basin,theHuobusun depression with a maximum depth of ∼12,000m[1,2].The Emonike upheaval is the front of the north Qaidam thrust belt,and exposes largelyDevonian volcanic detritus and sea shelf limestone withsome Carboniferous sandstone and limestone and Ju-rassic sandstone and mudstone with coals(Fig.2).Fieldobservations and seismic data show that the backthrustsF4and F3of front thrust F7have caused a south tilteddepression,the south Olonbuluk depression.The long-axis of the depression deepens southwestwards with amaximum depth of3500–400m occurring in the area ofthe Tuxi to Wulan anticlines to the southeast of Tuosu Hu(Lake)(Figs.2and3).These data further show that theOlonbuluk upheaval is a thin bedrock slab that wasprobably also uplifted by the larger backthrust F2of frontthrust F7.This fault backthrusts the southern margin ofthe Delingha depression northward,to face the oppositethrust fault F1that thrusts the northern margin of theDelingha depression southward.This tectonic activityhas probably given rise to the formation of the very deepNWW–SEE trending Delingha depression(∼3687km2)that contains Cenozoic sediments that are over6000mthick(Figs.2and3).Furthermore,the strong back-thrusting of F2has caused the backward propagationfault F2that thrusts and folds the Cenozoic stratigraphyto the north of the Olonbuluk Shan to form the Kelukeanticline(Figs.2and3).The Cenozoic stratigraphy in the Qaidam Basin hashistorically been divided into six formations with as-signed ages.These are(in upward sequence)the LuleheFm.(Paleocene to Eocene,E1–2),the Xia GanchaigouFm.(Oligocene,E3),the Shang Ganchaigou Fm.(earlyMiocene,N1),the Xia Youshashan Fm.(mid Miocene,N21),the Shang Youshashan Fm.(late Miocene,N22),theShizigou Fm.(Pliocene,N23)and the Qigequan Fm.(early Pleistocene,Q1).This age assignment is largelybased on pollen and ostracode analyses and has beenwidely accepted for geologic and tectonic studies and295X.Fang et al./Earth and Planetary Science Letters258(2007)293–306F i g .2.G e o l o g i c m a p o f t h e e a s t e r n p a r t o f t h e n o r t h Q a i d a m m a r g i n a l t h r u s t s h o w i n g t h e f a u l t s y s t e m a n d l o c a t i o n s o f t h eH u a i t o u t a l a s e c t i o n a l o n g t h e n o r t h l i m b o f t h e K e l u k e a n t i c l i n e .S e e F i g .1f o r i t s l o c a t i o n .S o l i d r e d l i n e :s u r f a c e f a u l t ;b r o k e n r e d l i n e :s u b -s u r f a c e f a u l t g i v e n b y s a t e l l i t e i m a g e s a n d s e i s m o s t r a t i g r a p h y .296X.Fang et al./Earth and Planetary Science Letters 258(2007)293–306lithostratigraphic correlation [1–3].The Lulehe Fm.is only found in the western Qaidam Basin along the margins of the Qiman Tagh –Kunlun Shan,the Altyn Tagh and the Nan Shan.The lithology is predominant-ly purple red and dark red alluvial conglomerate and gravelly sandstone intercalated with some sandy mud-stone and siltstone along the basin margin and a distal facies of shallow lake siltstone and mudstone toward the basin center.It superimposes unconformably upon Early Cretaceous and other older rocks.The Xia Ganchaigou Fm.has a larger distribution area than the Lulehe Fm.and is characterized by alternate brown red alluvial to fluvial conglomerate,gravelly sandstone and brown,yellow-green sandy mudstone in the lower part and playa brown siltstone and gray mudstone in the up-per part with thick salt and gypsum deposits in the depocenter close to the Altyn Tagh fault.The Shang Ganchaigou Fm.covers the whole basin and is largely interbedded multi-colored (brown to gray-green)lacus-trine sandstone,siltstone and mudstone intercalated with marl and nodular limestone.The Xia Youshashan Fm.appears over the entire basin and consists largely of gray yellow and brown sandstone to mudstone with some oolite marl at the basin center and fine conglomerate and sandstone at the basin margin.The Shang Youshashan Fm.is dominated by gray/yellow-green and light brown conglomerate,gravelly sandstone,siltstone and mud-stone.It contacts conformably with the underlying Xia Youshashan Fm.at the basin center but unconform-ably at the basin margins,especially along the western margin.The Shizigou Fm.is mostly conglomerate to sandstone intercalated with siltstone in the basin margin and yellow-gray calcareous sandy mudstone intercalat-ed with blue-gray sandstone and gravely sandstone.It also contacts conformably with the underlying Shang Youshashan Fm.at the basin center butunconformablyFig.3.Cross-section of A –B in Fig.2with locations for fossil mammal sites.Note the lower part of fault is mostly schematic and is not plotted in real vertical scale;the profile is vertically exaggerated;selected dip directions and dips are shown.297X.Fang et al./Earth and Planetary Science Letters 258(2007)293–306at the basin margins.The Qigequan Fm.is a distinc-tively thick gray conglomerate intercalated with sand-stone and sandy siltstone–mudstone covering most of the basin.Only in the depocenter at the middle to eastern part of the basin does it change to dark gray mud-stone intercalated with siltstone and muddy sandstone [1,2,24].Our paleomagnetic section lies along the north-ern limb of the Keluke anticline against the northern edge of the Olonbuluk Shan,about10km south of Huaitoutala Town(Fig.2).It is a4570-m exposed outcrop of the middle Miocene to Quaternary sedi-mentary rocks consisting of the Xia Youshashan Fm., Shang Youshashan Fm.,Shizigou Fm.and Qigequan Fm.(Fig.3).The Xia Youshashan Fm.has an exposure of only100m,characterized by fine-grained sedi-mentary rocks of siltstone,mudstone and marl.The Shang Youshashan Fm.is2250m thick(from100m to 2350m)and consists mainly of conglomerate and sandstone intercalated with siltstone for most of the stratigraphy and siltstone and mudstone in the upper-most part.The Shizigou Fm.is1750m thick(from 2350m to4100m),and is dominated by thick sand-stone intercalated with some mudstone.The Qigequan Fm.is only470m thick and is mainly conglomerate intercalated with thin sandy siltstone and mudstone (Fig.8a).3.Sampling and measurementsOriented block samples of roughly10×10×8cm were taken at intervals of2–5m depending on the availability of a suitable lithology at each level(site). These block samples were then cut into three oriented cubic specimens of2×2×2cm in the laboratory to form three parallel sets of samples for cross-calibration mea-surements.A total of1650block samples and1650×3 specimens were obtained.Systematic stepwise thermal demagnetizations(in fifteen to twenty discrete steps between∼25°C and 690°C at intervals of50°C below550°C and10–20°C above it)were done on the first set of specimens and the240pilot samples of the second set of the speci-mens.Remanent intensities and directional measure-ments were done on a2G Enterprises magnetometer in a magnetically shielded room,first in the Paleomag-netism Laboratory of the Institute of Geology and Geophysics(Chinese Academy of Sciences)and the Paleomagnetic and Rock Magnetic Laboratory of the Key Laboratory of Western China'sEnvironmentalSystems (Ministry of Education of China)in Lanzhou University,and then at the Graduate School of Ocean-ography,University of Rhode Island.Based on these results,only six to eight steps for temperatures between 350°C and 675°C were applied to the remaining specimens of the second set.The intensity of the natural remanent magnetization (NRM)of the clastic sedimentary samples is 1.5×10−2to 1.6×10−3A/m for mudstone and siltstone,and 0.6×10−2to 0.8×10−3A/m for sandstone.Representa-tive thermal demagnetization diagrams are shown in Fig.4.Most samples show simple demagnetization behavior.Below 50–100°C,a viscous remanent mag-netization (VRM)is readily removed (Fig.4).Between 100and 120°C,many samples show a clear decrease in magnetization ,accompanied by a clear change of rem-anent direction that indicates the removal of a second-ary remanent magnetization (SRM)stored by goethite (Fig.4a,b,c).Most samples show a low unblocking temperature component that can be removed easily at 250°C (Fig.4).Above this temperature,a characteristic magnetization (ChRM)is clearly isolated and decays nearly linearly to the origin.Three obvious rapid decays of the magnetization were observed for most samples at about 350°C,580°C and 660–690°C,indicative of the presence of maghemite,magnetite and hematite that act as major ChRM-carriers (Fig.4).ChRM component directions have been calculated for all samples using Principal Component Analysis.Rem-anence directions of the specimens generally agreed between the three laboratories unless the specimens were unstable and showed noisy demagnetization behavior (∼10%of the total,mostly from coarse sandstones).The final ChRM direction at each site was obtained by Fisher averaging of the directions from the two sets of spec-imens.Specimens not included in our magnetostrati-graphic analysis were rejected based on three criteria.(1)ChRM directions could not be determined because of ambiguous or noisy orthogonal demagnetization dia-grams.(2)ChRM directions revealed maximum angular deviation (MAD)angles greater than 15°.(3)Speci-mens revealed magnetizations with virtual geomagnetic pole (VGP)latitude values less than 30°.A total of 495horizontal levels in the column (30%)were excluded.The final remanent directions are averaged for each level and then are used to calculate VGPs that are plotted as a function of thickness after various paleomagnetic tests (Figs.5–7).Fig.5.(a)Equal-area projections of the characteristic remanent magnetization (ChRM)directions and mean directions (with oval of 95%confidence)for the Huaitoutala section determined with the bootstrap method (Tauxe [25]).Downward (upward)directions are shown as filled (open)circles.(b)Bootstrap reversal test diagram.Reversed polarity directions have been inverted to their antipodes to test for a common mean for the normal and reversed magnetization directions.The confidence intervals for all components overlap,indicating a positive reversal test.(For interpretation of the references to colour in this figure legend,the reader is referred to the web version of this article.)299X.Fang et al./Earth and Planetary Science Letters 258(2007)293–3064.MagnetostratigraphyAll the accepted ChRM directions of the Huaitoutala section from the Keluke anticline are used for a reversal test after tilt correction.An equal area projection of these ChRM directions shows that they record signals from the dipole of the earth's magnetic field(Fig.5a).A statistical bootstrap technique[25]has been used to test whether the distributions of the ChRM vectors are possibly non-Fisherian,and to characterize the associ-ated uncertainties for both normal and reversed ChRM directions(Fig.5b).The histograms of the Cartesian coordinates of bootstrapped means[25]allow us to determine a95%level of confidence(ovals around the means in Fig.5a)and to demonstrate that the bootstrap reversal test is positive(Fig.5b).The large change in bedding tilt along the section nearly orthogonally transecting the north limb of the Keluke anticline(Fig.3)provides an opportunity for a fold test[26,27].248representative high quality (MAD b5)site-mean ChRMs from different parts of the section were used for a calculation by the method of McElhinny[26],which indicates a positive fold test with the tilt-dependent dispersed ChRM directions tending to cluster together around their antipolar means(Fig.6).Furthermore,a jackknife technique[28]was used to quantify the reliability of the magnetostratigraphy.The jackknife parameter(J)obtained for the accepted spec-imen-mean directions has a value of−0.3,which falls within the range of0to−0.5recommended for a robust magnetostratigraphic data set by Tauxe and Gallet[28]. This result indicates that sampling of the section has recovered more than95%of the true number of polarity intervals(Fig.7).Fig.8shows a thickness vs.VGP plot of all the accepted and tested ChRM directions.It shows that there are a total of33normal and33reversed polarity intervals recorded in the Huaitoutala section,marked as N1–N33 and R1–R33,respectively(Fig.8).The observed po-larities can be correlated well with chrons2n-5Br of the Geomagnetic Polarity Time Scale(GPTS)of Cande and Kent[29]for most of the section.First,the strikingly long normal intervals N3–N4,N18and N29–31can be readily correlated to the characteristic longnormal Fig.6.Diagram showing a positive fold test of the248representative high quality site-mean ChRMs from different parts of the section using method by McElhinny[26].(For interpretation of the references to colour in this figure legend,the reader is referred to the web version of this article.) 300X.Fang et al./Earth and Planetary Science Letters258(2007)293–306chrons 2n (the Gauss Normal Polarity Chron),5n and 5ACn-5ADn,respectively.Then,the short normal inter-vals N5–N8of nearly equal duration are straightfor-wardly correlated to the four short normal events of chron 3n in the Gilbert Reversed Polarity Chron,as the Cochiti,Nunivak,Sidufjall and Thvera subchrons,respectively (Cande and Kent [29]);N9–10to chron 3An;N13–14,N16,N21–22,N27–28and N32–33to chron 4n,4An,5An,5ABn and 5ABn,respectively (Fig.8).The two clearly normal intervals N1and N2at the top of the section are regarded as analogs of the Reunion and Olduvai subchrons (2r.1n and 2n)in the Matuyama Reversed Polarity Chron,because of the persistent occurrence of very coarse sedimentary rocks (conglomerate and coarse sandstone)that indicate a fast depositional rate (Fig.8).Thus,the whole section was estimated to have formed between about 15.7Ma and 1.8Ma.The fossil mammals found in the lower,middle and upper parts of the section provide robust constraints on our interpretation of the observed polarities.These mammals fall into three faunas in the middle Miocene,late Miocene,and early Pliocene,respectively (Wang et al.,in preparation)(Table 1and Fig.8b).The Olonbuluk Fauna contains species of primitive deer Lagomeryx and Stephanocemas ,as well as rhinos such as Acerorhinus tsaidamensis [15].These taxacommonly occur in the middle Miocene of north China and are typical elements of the Tunggurian Land Mammal Age [30].The Tuosu Fauna features possibly the earliest occurrence of a Hipparion horse [16],as well as left over elements from the middle Miocene such as the Dicroceros deer.Presence of the three-toed horse undoubtedly indicates a late Miocene age and the Tuosu Fauna thus falls in the Baodean Land Mam-mal Age.The Huaitoutala Fauna currently contains small mammals only.It contains such typical Pliocene north China components as Orientalomys/Chardi-nomys and Mimomys and belongs to the Yushean Land Mammal Age.Thus defined,the lower Olonbu-luk Fauna is estimated to occur in 12.5–13.8Ma,the middle Tuosu Fauna at ∼11.4–9.5Ma,and the upper Huaitoutala fauna at ∼4.8Ma (Fig.8).Fig.9presents a thickness-vs.-age plot of the main chrons.It shows a linear relationship between the sam-pling thicknesses and chron ages that agrees to a first order (long-term change)with the lithologic change,which lends further support to our interpretation.Thus,the complete Shang Youshashan Fm.and Shizigou Fm.are determined to have formed in the intervals 15.3–8.1Ma and 8.1–2.5Ma,respectively.The Xia Youshashan Fm.and Qigequan Fm.are older and younger than 15.3Ma and 2.5Ma,respectively.5.Tectonic implicationsBased on the magnetostratigraphy,the average sedi-mentation rate of the Huaitoutala section was calculat-ed at about 33cm/ka.This very high rate is punctuated by three large persistent increases that started at about 14.7Ma,8.1Ma and 3.6Ma.We interpret these un-usually high sedimentation rate changes as records of three episodes of rapid tectonic uplift and fast exhu-mation and denudation (events T1to T3)of the NE Tibetan Plateau for the following reasons (Fig.9).First,early Cenozoic sedimentation rates are estimated at about 4–8cm/ka in the Qaidam Basin and the Tarim and Hexi Corridor Basins to the west and north of the Qilian Shan [31–33],and as low as ∼2–3cm/ka in the Xining Basin in the eastern Qilian Shan and Lanzhou –Linxia Basins [34–37](see Fig.1for localities).Sec-ond,in the late Cenozoic,sedimentation rates in these areas are generally three to four times higher than the early Cenozoic [33,36,38,39]with maximum rates over 70–80cm/ka clearly associated with tectonic defor-mation and uplift in the Gonghe –Guide Basin and Tarim Basin [40,41](Fig.1).Third,the late Cenozoic sedimentation rate increase also broadly agrees with the tectonic evolution of a late rapid deformation andupliftFig.7.Magnetostratigraphic jackknife analysis (Tauxe and Gallet [28])for the Huaitoutala section.The plot indicates the relationship between average percent of polarity zones retained and the percentage of sam-pling sites deleted,where the slope J is directly related to the robustness of the results.The obtained slopes J have values of −0.3032in the study section,which predicts that the section has recovered more than 95%of the true number of polarity intervals.301X.Fang et al./Earth and Planetary Science Letters 258(2007)293–306Fig.8.Magnetostratigraphic results versus lithostratigraphic position for the Huaitoutala section.Sites and main components of fossil mammals found along the section are plotted on the right side of the stratigraphic column for general age constraint.Identification of the mammals and their significance will be published by another paper by Xiaomin Wang and others.VGP:virtual geomagnetic polarity;GPTS:geomagnetic polarity time scale of Cande and Kent [29].Shaded polarity:suspected polarity most likely due to not sampling of a fresh surface.302X.Fang et al./Earth and Planetary Science Letters 258(2007)293–306of the NE Tibetan Plateau from models,basin analysis and thermochronology[3,7,8,10,13,18,23,36,41–45].Specific evidence for event T1includes field obser-vations of the Honggouzi anticline in the northwest Qaidam Basin(Fig.1)and seismostratigraphy of the Qaidam Basin demonstrate quite clearly that an uncon-formity occurs between the Shang Youshashan and Xia Youshashan Fms.close to the south slope of the Altyn Tagh and north margin of the Qaidam Basin.In our section,the first increase of sedimentation rate is also at the boundary of the Shang Youshashan and Xia Youshashan Fms.at15.3Ma accompanied by sharp changes in lithology from mostly fine sedimentary rocks of calcareous siltstone,mudstone and marl to predom-inantly coarse sedimentary rocks of sandstone interca-lated with conglomerate(Figs.8and9).In addition, rapid cooling of the rocks due to fast exhumation of the Qilian Shan and rapid rotation of the Guide Basin just east of the Qaidam Basin are recorded since the mid Miocene[46,47].Specific evidence for event T2at∼8.1Ma starts at the bottom of the Shizigou Fm.and is characterized by an upward increase of thick sandstone in the section (Fig.8),and of conglomerate in other sections over the margin of the Qaidam Basin.The predominance of alternating conglomerate and sandstone is the most marked feature of the Shizigou Fm.in the basin,and is indicative of rapid uplift of the surrounding moun-tains[1,2].A number of tectonic deformation and uplift events at∼8Ma have been reported around the Qaidam Basin and from various parts of the Tibetan Plateau,e.g.the Guide and Linxia Basins for the uplift of the east Kunlun Shan and west Qin Ling(Mts.) [36,41](see Fig.1for locations);the Jiuquan Basin in the west Hexi Corridor for the uplift of the north Qilian Shan[44,48];the Altyn Tagh from thermochronology [43,45];the Kuche depression for uplift of the Tien Shan[33];the Longmen Shan for uplift of east Tibet [49,50];and the Yangbajing Basin for uplift of south Tibet[51].The third sedimentation rate increase(event T3) at3.6Ma is not accompanied by a sharp lithologic change in the study section(even though the Quater-nary section is completely dominated by conglom-erate)(Figs.8and9),but is synchronous with the occurrence of a growing stratum dipping from67°to 45°within a narrow interval.This stratum is clearly indicative of a synchronous folding of the Keluke anticline by a backward propagation fault F2from backthrust F2due to a push by the southern Qilian Shan (Figs.1and3).Seismostratigraphy confirms that this growth stratum is an overall feature around all margins of the Qaidam Basin[1,2].An eastward fast shift of the depocenter of the Qaidam Basin was estimated to occur largely since the Plio-Quaternary[1,2,42].Just to the north side of the Qilian Shan,an unconformity caused by the strong deformation from the Qilian Shan was paleomagnetically dated at∼3.7Ma[44].Huge and thick boulder conglomerate due to a tectonic uplift first appeared at about this time around the rim of the whole Tibetan Plateau[38,41,44,48,52,53],although a con-current climatic change may also have contributed to this abrupt change[54].Initiation of an E–W extension and graben system in northern Tibet and the formation of the Kunlun Pass Basin due to the strike–slip of the Kunlun fault and other strike–slip faults,and the basaltic eruption and fast cooling of granites on the eastern Tibetan Plateau due to rapid tectonic uplift and exhumation are all reported to occur at about this time [48,55–58].The end of sedimentation in the study section at about1.8Ma is regarded as the strongest tectonic deformation due to the fast backward propagation of F2 driven by rapid backthrusting of F2,leading to the formation of the Keluke fault-propagation anticline. This anticline seems to be forming a clear step cutting the north limb of the anticline to the present.This fastTable1Mammalian faunas found in the Huaitoutala magnetic section and the nearby Tuosu Nor sectionName of fauna and component Suggested age Olongbuluk Fauna Middle Miocene(12–15Ma) Acerorhinus tsaidamensis,CD9825Lagomeryx tsaidamensis,CD9811,CD9818Stephanocemas sp.,CD9818Tuosu Fauna Late Miocene(10–12Ma) Dicroceros sp.,CD9815Euprox sp.,CD9820?Qurliknoria sp.,CD9824Chalicotherium brevirostris,CD9823Cervidae indet.,CD9824Artiodactyla indet.,CD9816Proboscidea indet.,CD9816Huaitoutala Fauna Early Pliocene(4–5Ma) Mimomys sp.,CD9822Orientalomys/Chardinomys sp.,CD9822Micromys sp.,CD9822Pseudomeriones sp.,CD9822Soricidae indet.,CD9822Numbers following taxonomic names are field numbers of the Institute of Vertebrate Paleontology and Paleoanthropology.For a more complete faunal list that includes mammals from other sections,see Wang et al.(in review).。

2007年全国大学生数学建模竞赛A题优秀论文—人口预测模型

中国人口预测模型摘要本文对人口预测的数学模型进行了研究。

首先，建立一次线性回归模型，灰色序列预测模型和逻辑斯蒂模型。

考虑到三种模型均具有各自的局限性，又用加权法建立了熵权组合模型，并给出了使预测误差最小的三个预测模型的加权系数，用该模型对人口数量进行预测，得到的结果如下：其次，建立Leslie人口模型，充分反映了生育率、死亡率、年龄结构、男女比例等影响人口增长的因素，并利用以1年为分组长度方式和以5年为负指数函数，并给出了反映城乡人口迁移的人口转移向量。

最后我们BP神经网络模型检验以上模型的正确性关键字：一次线性回归灰色序列预测逻辑斯蒂模型Leslie人口模型BP神经网络一、问题重述1. 背景人口增长预测是随着社会经济发展而提出来的。

在过去的几千年里，由于人类社会生产力水平低，生产发展缓慢，人口变动和增长也不明显，生产自给自足或进行简单的以货易货，因而对未来人口发展变化的研究并不重要，根本不用进行人口增长预测。

而当今社会，经济发展迅速，生产力达到空前水平，这时的生产不仅为了满足个人需求，还要面向社会的需求，所以必须了解供求关系的未来趋势。

而人口增长预测是对未来进行预测的各环节中的一个重要方面。

准确地预测未来人口的发展趋势，制定合理的人口规划和人口布局方案具有重大的理论意义和实用意义。

2. 问题人口增长预测有短期、中期、长期预测之分，而各个国家和地区要根据实际情况进行短期、中期、长期的人口预测。

例如，中国人口预期寿命约为70岁左右，因此，长期人口预测最好预测到70年以后，中期40—50年，短期可以是5年、10年或20年。

根据2007年初发布的《国家人口发展战略研究报告》（附录一）及《中国人口年鉴》收集的数据（附录二），再结合中国的国情特点，如老龄化进程加速，人口性别比升高，乡村人口城镇化等因素，建立合理的关于中国人口增长的数学模型，并利用此模型对中国人口增长的中短期和长期趋势做出预测，同时指出此模型的合理性和局限性。

Word2007文档的规范化操作方法

Word2007文档的规范化操作方法
战车
【期刊名称】《网络与信息》
【年(卷),期】2008(022)011
【摘要】在日常使用Word2007的过程中，我们应该尽量地能规范Word2007文档。

这样不仅便于浏览，而且也使得文档看上去更加美观。

如果你需要将Word2007打印或者编订的话，符合规范的文档就显得非常的重要。

规范的文档制作并非是困难的，只要你能掌握一些小技巧。

【总页数】1页(P73)
【作者】战车
【作者单位】无
【正文语种】中文
【中图分类】TP317.4
【相关文献】
1.没装Word2007一样查看X文档 [J], 一江春水
2.Word2007文档保存那些事儿 [J], 王霞
3.用word2007快速生成文档目录 [J], 王桂兰
4.Word2007在长篇文档编辑中的几个技巧 [J], 楚叶峰;周海涛
5.Word2007文档＂通配符＂巧＂替换＂ [J], 王杰
因版权原因，仅展示原文概要，查看原文内容请购买。

中队论文 Microsoft Office Word 文档

如何有效帮助单亲家庭中的问题学生健康成长姓名：焦金欢学校：县一小近几年，随着社会中离婚率的逐年攀高，单亲家庭数量的上升，单亲家庭子女的教育问题已经成了一个社会问题，父母的离异，让很多孩子承担了原不该属于自己这个年龄的痛苦。

诸多单亲孩子内心的伤痛，给社会带来了新的问题，也给我们教育工作者带来了许多困难。

由于这些孩子处在一个特殊的家庭结构里，他们在思想、学习、性格，甚至健康方面在一定程度上都有别于完整家庭的子女，具有一定的特殊性。

如何认识这种特殊性，怎样有针对性地对单亲家庭的学生进行教育，不仅许多单亲家庭的父母对此茫然失措，学校也是“老兵遇着新问题”，社会目前也缺乏有效的特别是有针对性的指导。

所以在这个时候，我对“如何有效帮助单亲家庭中的问题学生健康成长”这个问题进行了进一步的探究。

希望通过个案的研究找到单亲家庭学生的一些特殊的共性，给予单亲家庭的父母一些有规律的方法，对孩子进行行之有效的指导，从而让他们健康的成长。

作为辅导员，我主要针对“形成单亲家庭问题学生的原因，以及如何帮助这些孩子抚平心理创伤。

”做些有目的的探索，主要是争取把健康的家庭教育的理念、家庭教育方法以及教育孩子成长的有效途径渗透给家长，走出由于父母离异给自己带来的心灵困惑，和同龄孩子一样，用健康的心态去迎接学习、生活的新挑战。

通过对单亲家庭中的问题学生的调查研究、探索总结，我对“如何有效帮助单亲家庭中的问题学生健康成长”，也有了一些小小的收获。

一．用爱心去弥补受伤的心灵。

单亲家庭的孩子在家庭遇到变故时，往往心灵受伤，从而关闭与同学、老师交流的窗户。

爱是打开他们心扉的钥匙，是缝合心灵创伤的灵丹妙药。

我从他们忧郁的眼神里，看到了一颗受伤的心，一颗渴望家庭温暖的心，一颗渴望大家关爱的心。

老师和同学都关心他们，愿意帮助他们。

精诚所致，金石为开”。

在老师，同学，校领导的关爱下，他们最终会走出心灵的阴影，露出了盈盈笑脸。

二不断鼓励与表扬去增强自信。

基于Word2007批量文件的设计与实现

基于Word2007批量文件的设计与实现
史军绒
【期刊名称】《科技信息》
【年(卷),期】2011(0)29
【摘要】本文针对在实际工作中经常遇到的象制作信函、电子邮件、信封、标签等操作起来方法一样但重复工作量很大的工作,给出了利用Word2007进行批量文档制作的流程图,并且通过实例论述了运用邮件合并,完成批量文档制作的方法.【总页数】2页(P656,691)
【作者】史军绒
【作者单位】陕西理工学院图书馆陕西汉中723003
【正文语种】中文
【相关文献】
1.基于WinSocket的大文件批量传输系统的设计与实现
2.批量导入文件名功能模块设计与实现
3.一种图像文件批量换名软件的设计与实现
4.基于FME的DWG文件批量坐标转换设计与实现
5.批量文件处理软件的设计与实现
因版权原因，仅展示原文概要，查看原文内容请购买。

第十一届湖北省自然科学优秀学术论文评审表(一等奖)

武汉大学
湖北省水利学会
6
Lys691 and Asp714 of the Na+/K+-ATPase alpha subunit are essential for phosphorylaiton, dephosphorylation, and enzyme turnover
苏萍
2004年4月美国化学会Biochemistry杂志上（SCI收录）
华中科技大学系统工程研究所
湖北系统工程学会
12
糖姜片的无硫的护色及加工工艺研究
莫开菊
汪兴平
程超
2005《农业工程学报》第1期155-158（EI收录）
湖北民族学院
农产品加工与贮藏工程
华中农业大学
湖北省园艺学会
4
Production and characterization of somatic hvbrids between upland cotton (Gossypium hirsutum) and wild cotton (G.klotzschianum Anderss)via electrofusion
33472005sciei收录欧洲运筹学europeanjournalofoperationalresearch2004年总第157期第372388页sciei收录武汉理工大学自动化学院湖北省系统工程11agametheoreticalcooperativemechanismdesigntwoechelondecentralizedsupplychainfora王红卫郭敏华中科技大学系统工程研究所湖北系统工程学会12糖姜片的无硫的护色及加工工艺研究莫开菊汪兴平程超2005农业工程学报第1期155158ei收录湖北民族学院农产品加工与贮藏工程

科学文献

State Key Laboratory of Software Engineering, Wuhan University Wuhan 430072, P.R.China
Abstract
The classical methods for model building are usually based on the parameters selection for xed model form. In this paper, we use a method based on natural genetic evolution for a practical problem in engineering geologics. Several useful and interpretable models are obtained in some runs. It is e cient for the prediction and decision in searching the optimal model .
2 Evolutionary Model-Building
To build a model means to provide a convenient conceptual representation of the observed system from examples. It is on the model which we use to think about the true situation that interpretations, predictions, and decisions would be based. The quality of a model is measured by an objective function , which is related to the discrepancy of the observed values fyi g from the expected values ff (xi )g and is normally induced by a distance function 4] . Genetic algorithms ( GAs ) , rst speci ed by John Holland in the early seventies, are becoming an important tool in optimization problems and machine learning. GAs are adaptive search strategies based on a highly abstract model of biological evolution. Coding techniques and selection mechanisms are two major parts in a GA. Population size is an important parameter to consider when applying a GA to a particular problem. Compare with the classical optimal algorithms, GAs have several speci c characters. A GA deals with codes of individuals, not the individuals themselves. A GA maintains a population of individuals, not an individual one time. A GA uses much less auxiliary information for tness than classical methods and it probabilistically modi es the population by some genetic operators. The four fundamental steps in a GA are as following: To determine a representation scheme, To determine a measure for tness, To determine the parameters and variables to control the algorithms, To determine the stop criterion algorithm.

2007年毕业论文

--------------------------------------------------------------------------------------------------------------------------------------------广州X X X X X职业学院毕业设计（论文）论文题目:试析广州花园酒店的市场营销研究--———广州花园酒店的市场营销研究系别：________ __财经系___________专业名称: _________市场营销__________姓名： ____________________学号: ________________指导老师： _________ ______________完成时间: _________2006年12月5号____---------------------------------------------------------精品文档-----------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------摘要进入21世纪以来中国的酒店业经营遇到了许多问题,但随着经济的飞速发展,酒店业的发展趋势是不可阻挡的.广州花园酒店，执业界之牛耳，从1985年开业至今，享誉中外二十载，是目前国内最具有规模的五星级商务酒店。

邓小平同志还曾为花园酒店亲笔题写店名。

为了提高市场营销研究能力，本文试就在新形势下对广州花园酒店进行市场营销研究，在酒店环境、发展状况基础上进行企业行为分析；并运用常用管理方法:服务质量管理、收益管理、危机管理等和经营战略：产品、价格、促销策略，把酒店的服务产品、收益、价格等进行定位分析、细分、目标市场选择和战略选择，（这句话好像不是很通顺）并在2006年的广交会中分析酒店---------------------------------------------------------精品文档-----------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------国际化经营战略，从而提高自己对市场的分析能力，并提出对酒店发展的建议展望。

2007 Office：箭在弦上

2007 Office：箭在弦上
陈琼
【期刊名称】《互联网周刊》
【年(卷),期】2006(000)028
【摘要】作为重量级仅次于Windows Vista的拳头产品，即将于年底亮相的新版本Office软件，同样寄托着微软谨慎而又复杂的情绪
【总页数】1页(P54)
【作者】陈琼
【作者单位】《互联网周刊》记者
【正文语种】中文
【中图分类】TP317.1
【相关文献】
1.Office 2003和Office 2007版本特点分析 [J], 姜立
2.高版本照样能打开——用Office 2003打开Office 2007文件 [J], 马玉明
3.遗留Office环境中的Office 2007安全特性 [J], Russell Smith; 欧阳宇（译者）
4.认识Office2007 Microsoft Office 2007答疑 [J], Dan; Holme; 黄思维（译）
5.Office Server 初探：认识Office 2007——Dan Holme就Microsoft
Office2007的一些常见问题为您答疑解惑 [J], Dan;Holme;黄思维（译）
因版权原因，仅展示原文概要，查看原文内容请购买。