latex 演示文档模板
latex英文模板

\documentclass{article}\usepackage{graphicx}\usepackage[round]{natbib}\bibliographystyle{plainnat}\usepackage[pdfstartview=FitH,%bookmarksnumbered=true,bookmarksopen=true,%colorlinks=true,pdfborder=001,citecolor=blue,%linkcolor=blue,urlcolor=blue]{hyperref}\begin{document}\title{Research plan under the Post-doctorate program at xx University}%\subtitle{aa}\author{Robert He}\date{2008/04/23}\maketitle\section{Research Title}~~~~Crustal seismic anisotropy in the xx using Moho P-to-S converted phases.\section{Research Background \& Purposes}~~~~Shear-wave splitting analyses provide us a new way to study the seismic structure and mantle dynamics in the crust and mantle. The crustal anisotropy is developed due to various reasons including lattice-preferred orientation (LPO) of mineral crystals and oriented cracks.\newlineTraditionally, the earthquakes occurring in the curst and the subducting plates are selected to determine the seismic anisotropy of the crust. However, none of these methods can help us to assess the anisotropy in the whole crust. Because crustal earthquakes mostly are located in the upper crust, they do not provide information of lower crust. On the other hand, earthquakes in the subducting plates provide information of the whole crust but combined with upper mantle. However, it’s difficult to extract the sole contri bution of the crust from the measurement. Fortunately P-to-S converted waves (Ps) at the Moho are ideal for investigation of crustal seismic anisotropy since they are influenced only by the medium above the Moho.Moho. Figure \ref{crustalspliting}~schematically shows the effects of shear wave splitting on Moho Ps phases. Initially, a near-vertically incident P wave generates a radially polarized converted shear wave at the crust-mantle boundary. The phases, polarized into fast and slow directions, progressively split in time as they propagate through the anisotropic media. Here, the Ps waves can be obtained from teleseismic receiver function analysis.%%\begin{figure}[htbp]\begin{center}\includegraphics[width=0.47\textwidth]{crustalsplit.png}\caption{The effects of shear wave splitting in the Moho P to S converted phase. Top shows a schematic seismogram in the fast/slow coordinate system with split horizontal Ps components.(cited from: McNamara and Owens, 1993)}\label{crustalspliting}\end{center}\end{figure}%%The Korean Peninsula is composed of three major Precambrian massifs, the Nangrim, Gyeongii, and Yeongnam massifs(Fig.\ref{geomap}). The Pyeongbuk-Gaema Massif forms the southern part of Liao-Gaema Massif of southern Manchuria, and the Gyeonggi and Mt. Sobaeksan massifs of the peninsula are correlated with the Shandong and Fujian Massifs of China.%\begin{figure}[htbp]\begin{center}\includegraphics[width=0.755\textwidth]{geo.png}\caption{Simplified geologic map. NCB: North China block; SCB: South China block.(cited from: Choi et al., 2006)}\label{geomap}\end{center}\end{figure}%Our purpose of the study is to measure the shear wave splitting parameters in the crust of the Korean Peninsula. The shear wave splitting parameters include the splitting time of shear energybetween the fast and slow directions, as well as fast-axis azimuthal direction in the Korean Peninsula. These two parameters provide us constraints on the mechanism causing the crustal anisotropy. From the splitting time, the layer thickness of anisotropy will be estimated. Whether crustal anisotropy mainly contributed by upper or lower crustal or both will be determined. Based on the fast-axis azimuthal direction, the tectonic relation between northeastern China and the Korean peninsula will be discussed.\section{Research Methods}~~~~Several methods have been introduced for calculation of receiver functions. An iterative deconvolution technique may be useful for this study since it produces more stable receiver function results than others. The foundation of the iterative deconvolution approach is aleast-squares minimization of the difference between the observed horizontal seismogram and a predicted signal generated by the convolution of an iteratively updated spike train with the vertical-component seismogram. First, the vertical component is cross-correlated with the radial component to estimate the lag of the first and largest spike in the receiver function (the optimal time is that of the largest peak in the absolute sense in the cross-correlation signal). Then the convolution of the current estimate of the receiver function with the vertical-component seismogram is subtracted from the radial-component seismogram, and the procedure is repeated to estimate other spike lags and amplitudes. With each additional spike in the receiver function, the misfit between the vertical and receiver-function convolution and the radial component seismogram is reduced, and the iteration halts when the reduction in misfit with additional spikes becomes insignificant.\newlineFor all measurement methods of shear-wave splitting, time window of waveform should be selected. Conventionally the shear-wave analysis window is picked manually. However, manual window selection is laborious and also very subjective; in many cases different windows give very different results.\newlineIn our study, the automated S-wave splitting technique will be used, which improves the quality of shear-wave splitting measurement and removes the subjectivity in window selection. First, the splitting analysis is performed for a range of window lengths. Then a cluster analysis isapplied in order to find the window range in which the measurements are stable. Once clusters of stable results are found, the measurement with the lowest error in the cluster with the lowest variance is presented for the analysis result.\section{Expected results \& their contributions}~~~~First, the teleseismic receiver functions(RFs) of all stations including radial and transverse RFs can be gained. Based on the analysis of RFs, the crustal thickness can be estimated in the Korean Peninsula. Then most of the expected results are the shear-wave splitting parameters from RFs analysis in the crust beneath the Korean Peninsula. The thickness of anisotropic layer will be estimated in the region when the observed anisotropy is assumed from a layer of lower crustal material.All the results will help us to understand the crustal anisotropy source.\newlineCrustal anisotropy can be interpreted as an indicator of the crustal stress/strain regime. In addition, since SKS splitting can offer the anisotropy information contributed by the upper mantle but combined with the crust, the sole anisotropy of the upper mantle can be attracted from the measurement of SKS splitting based on the crustal splitting result.%\cite{frogge2007}%%%\citep{frogge2008}%%%\citep{s-frogge2007}% 5. References\begin{thebibliography}{99}\item Burdick, L. J. and C. A. Langston, 1977, Modeling crustal structure through the use of converted phases in teleseismic body waveforms, \textit{Bull. Seismol. Soc. Am.}, 67:677-691.\item Cho, H-M. et al., 2006, Crustal velocity structure across the southern Korean Peninsula from seismic refraction survey, \textit{Geophy. Res. Lett.} 33, doi:10.1029/2005GL025145.\item Cho, K. H. et al., 2007, Imaging the upper crust of the Korean peninsula by surface-wave tomography, \textit{Bull. Seismol. Soc. Am.}, 97:198-207.\item Choi, S. et al., 2006, Tectonic relation between northeastern China and the Korean peninsula revealed by interpretation of GRACE satellite gravity data, \textit{Gondwana Research}, 9:62-67.\item Chough, S. K. et al., 2000, Tectonic and sedimentary evolution of the Korean peninsula: a review and new view, \textit{Earth-Science Reviews}, 52:175-235.\item Crampin, S., 1981, A review of wave motion in anisotropic and cracked elastic-medium, \textit{Wave Motion}, 3:343-391.\item Fouch, M. J. and S. Rondenay, 2006, Seismic anisotropy beneath stable continental interiors, \textit{Phys. Earth Planet. Int.}, 158:292-320.\item Herquel, G. et al., 1995, Anisotropy and crustal thickness of Northern-Tibet. New constraints for tectonic modeling, \textit{Geophys. Res. Lett.}, 22(14):1 925-1 928.\item Iidaka, T. and F. Niu, 2001, Mantle and crust anisotropy in the eastern China region inferred from waveform splitting of SKS and PpSms, \textit{Earth Planets Space}, 53:159-168.\item Kaneshima, S., 1990, Original of crustal anisotropy: Shear wave splitting studies in Japan, \textit{J. Geophys. Res.}, 95:11 121-11 133.\item Kim, K. et al., 2007, Crustal structure of the Southern Korean Peninsula from seismic wave generated by large explosions in 2002 and 2004, \textit{Pure appl. Geophys.}, 164:97-113.\item Kosarev, G. L. et al., 1984, Anisotropy of the mantle inferred from observations of P to S converted waves, \textit{Geophys. J. Roy. Astron. Soc.}, 76:209-220.\item Levin, V. and J. Park, 1997, Crustal anisotropy in the Ural Mountains foredeep from teleseismic receiver functions, \textit{Geophys. Res. Lett.}, 24(11):1 283 1286.\item Ligorria, J. P. and C. J. Ammon, 1995, Iterative deconvolution and receiver-function estimation. \textit{Bull. Seismol. Soc. Am.}, 89:1 395-1 400.\item Mcnamara, D. E. and T. J. Owens, 1993, Azimuthal shear wave velocity anisotropy in the basin and range province using Moho Ps converted phases, \textit{J. Geophys. Res.}, 98:12003-12 017.\item Peng, X. and E. D. Humphreys, 1997, Moho dip and crustal anisotropy in northwestern Nevada from teleseismic receiver functions, \textit{Bull. Seismol. Soc. Am.}, 87(3):745-754.\item Sadidkhouy, A. et al., 2006, Crustal seismic anisotropy in the south-central Alborz region using Moho Ps converted phases, \textit{J. Earth \& Space Physics}, 32(3):23-32.\item Silver, P. G. and W. W. Chan, 1991, Shear wave splitting and subcontinental mantle deformation, \textit{J. Geophys. Res.},96:16 429-16454.\item Teanby, N. A. et al., 2004, Automation of shear wave splitting measurement using cluster analysis, \textit{Bull. Seismol. Soc. Am.}, 94:453-463.\item Vinnik, L. and J-P. Montagner, 1996, Shear wave splitting in the mantle Ps phases,\textit{Geophys. Res. Lett.}, 23(18):2 449- 2 452.\item Yoo, H. J. et al., 2007, Imaging the three-dimensional crust of the Korean peninsula by joint inversion of surface-wave dispersion of teleseismic receiver functions, \textit{Bull. Seismol. Soc. Am.}, 97(3):1 002-1 011.\item Zhu, L., and H. Kanamori, 2000, Moho depth variation in Southern California from teleseismic receiver functions, \textit{J. Geophys. Res.}, doi :10.1029/1999JB900322, 105:2 969-2 980.%%%%\end{document}。
Latex制作幻灯片PPT简易模板

Latex简介
Latex特点
支持高质量的排版和输出,具有丰富的数学符号和公式支持,可定制性强。
Latex与PPT比较
相对于传统的PPT制作软件,Latex制作的幻灯片在排版、数学公式和定制化方 面具有优势。
幻灯片制作概述
幻灯片构成
一般包括标题页、目录页、正文页和 结尾页等部分。
制作流程
确定主题和内容,选择合适的幻灯片模 板,编写和排版正文内容,插入图片和 表格等辅助材料,最后输出为PDF或 PPT格式进行展示。
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字体、字号、颜色
可以通过相应的命令和环境来 设置文本的字体、字号和颜色。
对齐方式
Latex提供了多种对齐方式,如 居中对齐、左对齐、右对齐等。
行距、段距
可以通过设置相应的参数来调 整文本的行距和段距,使幻灯
片更加美观易读。
列表与编号
Latex支持有序列表和无序列表, 并提供了多种编号方式,方便
使用背景与边框
背景图片
选择与主题相关的背景图片,增加视觉冲击力, 同时注意图片清晰度和版权问题。
背景色块
使用不同颜色或渐变色块作为背景,划分不同内 容区域,增加层次感。
边框装饰
为幻灯片添加边框或装饰元素,提升美观度和专 业感。
布局调整与优化
内容布局
合理安排文字、图片、 图表等元素的位置和大 小,保持整体协调性和
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Latex幻灯片基础
幻灯片类别与结构
幻灯片类别
beamer、powerdot、prosper等, 其中beamer最为常用。
帧(frame)概念
在Latex中,一个幻灯片页面被称为一 个帧,是制作幻灯片的基本单元。
(完整版)latex初学者模板

(完整版)latex初学者模板% a4paper - A4 纸 11pt - 字体 twoside - 双面 openany - 新章节可在偶数页开始\documentclass[a4paper,11pt,twoside,openany]{article} % ----------------------------- 纸张大小 ------------------------------------- % 定义转换成 pdf 文档的纸张大小,应与 \paperwidth \paperheight 一致 %\special{pdf: pagesize width 20cm height 30cm}% true 的含义是保持尺寸不会随一些参数的变化而变化,具体可见 Knuth 的 TeXbook % 纸张宽% 纸张高页面布局 --------% 正文宽%\textheight 20 true cm %\headheight 14pt %\headsep 16pt%\footskip27pt%\marginparsep 10pt %\marginparwidth 100pt % --------------------------- 页边空白调整\setlength{\evensidemargin}{0mm} % 置 0 \iffalse % 如果考虑右侧(书外侧)的边注区则改为\iftrue \addtolength{\evensidemargin}{\marginparsep}\addtolength{\evensidemargin}{\marginparwidth} \fi% \paperwidth = h + \oddsidemargin+\textwidth+\evensidemargin + h\setlength{\hoffset}{\paperwidth} \addtolength{\hoffset}{-\oddsidemargin} \addtolength{\hoffset}{-\textwidth} \addtolength{\hoffset}{-\evensidemargin}\setlength{\hoffset}{0.5\hoffset} \addtolength{\hoffset}{-1in}\setlength{\voffset}{-1in}\setlength{\topmargin}{\paperheight}%\paperwidth 20 true cm %\paperheight 30 true cm % ------------------------ %\textwidth 10 true cm % 正文高% 页眉高 % 页眉距离% 页脚距离 % 边注区距离 % 边注区宽\def\marginset#1#2{ \marginset{left}{top}\setlength{\oddsidemargin}{#1} \iffalse \iftrue\reversemarginpar\addtolength{\oddsidemargin}{\marginparsep}\addtolength{\oddsidemargin}{\marginparwidth} \fi% 页边设置% 左边(书内侧)装订预留空白距离% 如果考虑左侧(书内侧)的边注区则改为% h = \hoffset + 1in% 0 = \voffset + 1in\iffalse % 将这里改为 \iftrue 即可使用\ifx\pdfoutput\undefined % Not run pdftex % \ifx % \usepackage[dvips]{hyperref} % \else\addtolength{\topmargin}{-\headheight}\addtolength{\topmargin}{-\headsep}\addtolength{\topmargin}{-\textheight}\addtolength{\topmargin}{-\footskip}\addtolength{\topmargin}{#2}\setlength{\topmargin}{0.5\topmargin}% 上边预留装订空白距离}% 调整页边空白使内容居中,两参数分别为纸的左边和上边预留装订空白距离 \marginset{10mm}{12mm} % --------------------------- 字体支持 -------------------------\usepackage{times}字体% 使用 Times New Roman\usepackage{CJK,CJKnumb,CJKulem} % 中文支持宏包%\usepackage{ccmap} % 使pdfLatex 生成的文件支持复制等 %\usepackage[mtbold,mtpluscal,mtplusscr]{mathtime}% 数学环境用 Times New Roman% ---------------------------\usepackage{fancyhdr} \pagestyle{fancy}% --------------------------- \usepackage{color}\usepackage{indentfirst}%\setlength{\parindent}{2em}页眉页脚 -------------------------% 页眉页脚相关宏包 % 页眉页脚风格段落字体格式 ----% 支持彩色 % 首行缩进宏包% 段落缩进\setlength{\parskip}{0.7ex plus0.3ex minus0.3ex} %%\linespread{1.2}\renewcommand{\baselinestretch}{1.2} 段落间距% 行距倍数% 行距倍数(同上)\newcommand{\hei}{\CJKfamily{hei}}%黑体 \newcommand{\fs}{\CJKfamily{fs}}% 仿宋\newcommand{\kai}{\CJKfamily{kai}}%楷体 \newcommand{\li}{\CJKfamily{li}}% 隶书\newcommand{\you}{\CJKfamily{you}} %幼圆\newcommand{\wuhao}{\fontsize{10.5pt}{12.6pt}\selectfont} \newcommand{\xiaosi}{\fontsize{12pt}{14pt}\selectfont} \newcommand{\sihao}{\fontsize{14pt}{\baselineskip}\selectf ont} % %\marginparpush% 五号字体 % 小四字体四号字体%% --------------------------- 超链接和标签 ----------------------- %\renewcommand{\CJKglue}{\hskip 0pt plus 0.08\baselineskip} % 汉字字距% 自定义文字块例子%\newcommand{\aaa}{ 这是测试 }\newcommand{\song}{\CJKfamily{song}} % 宋体\usepackage[dvipdfm]{hyperref}% \fi \AtBeginDvi{\special{pdf:tounicode GBK-EUC-UCS2}} % GBK -> Unicode \else \usepackage[pdftex]{hyperref} \fi \hypersetup{CJKbookmarks,% bookmarksnumbered,% colorlinks,% linkcolor=blue,% citecolor=blue,% hyperindex,% plainpages=false,% pdfstartview=FitH} \fi% ------------------------------- 注释 --------------------------------------- \iffalse % 将这里改为 \iftrue 即可使用 %注释掉一段内容\usepackage{verbatim} \begin{comment}This is a comment example. \end{comment}\fi %\makeatletter % @ is now a normal "letter" for Tex%\makeatother % @ is restored as a "non-letter" for Tex % ------------------------------- 其他宏包------------------------ %\usepackage{amsmath,amsthm,amsfonts,amssymb,bm} % 数学宏包 %\usepackage{graphicx,psfrag} %\usepackage{makeidx} 包%\usepackage{listings} % ------------------------------- \begin{document} % 开始正文 % song- 宋体 hei- 黑体 fs- 仿宋 kai- 楷体 li- 隶书 you- 幼圆 com 为 song+hei\begin{CJK*}{GBK}{com}% 开始中文环境\CJKtilde % 重定义 ~代表的空白距离 \CJKindent首缩进\CJKcaption{GB} 节标题 \author{ceo}\title{ 一个 latex 例子 } \maketitle成标题%\thispagestyle{empty} % 设置首页的页眉页脚风格%\setlength{\baselineskip}{3ex plus1ex minus1ex} % 调整行距\TeX{}~ 是由图灵奖得主\index{Knuth, Donald E.}~Donald E. Knuth\cite{texbook}~ 编写的计算机程序,用于文章和数学公式的排版。
(完整版)latex初学者模板

% a4paper - A4 纸 11pt - 字体 twoside - 双面 openany - 新章节可在偶数页开始 \documentclass[a4paper,11pt,twoside,openany]{article}% ----------------------------- 纸张大小 ------------------------------------- % 定义转换成 pdf 文档的纸张大小,应与 \paperwidth \paperheight 一致 %\special{pdf: pagesize width 20cm height 30cm}% true 的含义是保持尺寸不会随一些参数的变化而变化,具体可见 Knuth 的 TeXbook % 纸张宽% 纸张高页面布局 --------% 正文宽%\textheight 20 true cm %\headheight 14pt %\headsep 16pt%\footskip27pt%\marginparsep 10pt %\marginparwidth 100pt % --------------------------- 页边空白调整\setlength{\evensidemargin}{0mm} % 置 0 \iffalse % 如果考虑右侧(书外侧)的边注区则改为 \iftrue \addtolength{\evensidemargin}{\marginparsep} \addtolength{\evensidemargin}{\marginparwidth} \fi% \paperwidth = h + \oddsidemargin+\textwidth+\evensidemargin + h\setlength{\hoffset}{\paperwidth} \addtolength{\hoffset}{-\oddsidemargin} \addtolength{\hoffset}{-\textwidth} \addtolength{\hoffset}{-\evensidemargin} \setlength{\hoffset}{0.5\hoffset} \addtolength{\hoffset}{-1in}\setlength{\voffset}{-1in}\setlength{\topmargin}{\paperheight}%\paperwidth 20 true cm %\paperheight 30 true cm % ------------------------ %\textwidth 10 true cm % 正文高% 页眉高 % 页眉距离% 页脚距离 % 边注区距离 % 边注区宽\def\marginset#1#2{ \marginset{left}{top}\setlength{\oddsidemargin}{#1} \iffalse \iftrue\reversemarginpar\addtolength{\oddsidemargin}{\marginparsep} \addtolength{\oddsidemargin}{\marginparwidth} \fi% 页边设置% 左边(书内侧)装订预留空白距离% 如果考虑左侧(书内侧)的边注区则改为% h = \hoffset + 1in% 0 = \voffset + 1in\iffalse % 将这里改为 \iftrue 即可使用\ifx\pdfoutput\undefined % Not run pdftex % \ifx % \usepackage[dvips]{hyperref} % \else\addtolength{\topmargin}{-\headheight} \addtolength{\topmargin}{-\headsep} \addtolength{\topmargin}{-\textheight} \addtolength{\topmargin}{-\footskip} \addtolength{\topmargin}{#2} \setlength{\topmargin}{0.5\topmargin}% 上边预留装订空白距离}% 调整页边空白使内容居中,两参数分别为纸的左边和上边预留装订空白距离 \marginset{10mm}{12mm} % --------------------------- 字体支持 -------------------------\usepackage{times}字体% 使用 Times New Roman\usepackage{CJK,CJKnumb,CJKulem} % 中文支持宏包 %\usepackage{ccmap} % 使 pdfLatex 生成的文件 支持复制等 %\usepackage[mtbold,mtpluscal,mtplusscr]{mathtime}%数学环境用 Times New Roman% ---------------------------\usepackage{fancyhdr} \pagestyle{fancy}% --------------------------- \usepackage{color}\usepackage{indentfirst}%\setlength{\parindent}{2em}页眉页脚 -------------------------% 页眉页脚相关宏包 % 页眉页脚风格 段落字体格式 ----% 支持彩色 % 首行缩进宏包% 段落缩进\setlength{\parskip}{0.7ex plus0.3ex minus0.3ex} %%\linespread{1.2}\renewcommand{\baselinestretch}{1.2} 段落间距% 行距倍数% 行距倍数(同上)\newcommand{\hei}{\CJKfamily{hei}}%黑体 \newcommand{\fs}{\CJKfamily{fs}}% 仿宋\newcommand{\kai}{\CJKfamily{kai}}%楷体 \newcommand{\li}{\CJKfamily{li}}% 隶书\newcommand{\you}{\CJKfamily{you}} %幼圆\newcommand{\wuhao}{\fontsize{10.5pt}{12.6pt}\selectfont} \newcommand{\xiaosi}{\fontsize{12pt}{14pt}\selectfont}\newcommand{\sihao}{\fontsize{14pt}{\baselineskip}\selectfont} % %\marginparpush% 五号字体 % 小四字体四号字体%% --------------------------- 超链接和标签 ----------------------- %\renewcommand{\CJKglue}{\hskip 0pt plus 0.08\baselineskip} % 汉字字距% 自定义文字块例子%\newcommand{\aaa}{ 这是测试 }\newcommand{\song}{\CJKfamily{song}} % 宋体\usepackage[dvipdfm]{hyperref}% \fi \AtBeginDvi{\special{pdf:tounicode GBK-EUC-UCS2}} % GBK -> Unicode \else \usepackage[pdftex]{hyperref} \fi\hypersetup{CJKbookmarks,% bookmarksnumbered,% colorlinks,% linkcolor=blue,% citecolor=blue,% hyperindex,% plainpages=false,% pdfstartview=FitH} \fi% ------------------------------- 注释 --------------------------------------- \iffalse % 将这里改为 \iftrue 即可使用 %注释掉一段内容 \usepackage{verbatim} \begin{comment}This is a comment example. \end{comment}\fi %\makeatletter % @ is now a normal "letter" for Tex%\makeatother % @ is restored as a "non-letter" for Tex % ------------------------------- 其他宏包 ------------------------ %\usepackage{amsmath,amsthm,amsfonts,amssymb,bm} % 数学宏包 %\usepackage{graphicx,psfrag} %\usepackage{makeidx}包%\usepackage{listings} % ------------------------------- \begin{document} % 开始正文 % song- 宋体 hei- 黑体 fs- 仿宋 kai- 楷体 li- 隶书 you- 幼圆 com 为 song+hei\begin{CJK*}{GBK}{com}% 开始中文环境\CJKtilde % 重 定义 ~代表的空白距离 \CJKindent首缩进\CJKcaption{GB} 节标题 \author{ceo}\title{ 一个 latex 例子 } \maketitle成标题%\thispagestyle{empty} % 设置首页的 页眉页脚风格%\setlength{\baselineskip}{3ex plus1ex minus1ex} % 调整行距\TeX{}~ 是由图灵奖得主 \index{Knuth, Donald E.}~Donald E. Knuth\cite{texbook}~ 编写的计算机程序,用于文章和数学公式的排版。
latex模板

latex模板Latex 实用例子通过实验本例子可以基本掌握科技排版的方法:\documentclass[twocolumn]{article}\usepackage{amsmath}\renewcommand{\rmdefault}{ptm}\begin{document}\title{ Measure the axes of nearby nitrogen-vacancy centers in diamond with polarized light}\author{ Jing-Ru Wang\\Department of physics,the Beijing University of Posts and Telecommunications}\date{November 17, 2015}\maketitle\begin{abstract}NV)center in diamond is an attractive The negatively charged nitrogen-vacancy(candidate because of their excellent spin and optical characteristics for quantum information and metrology. To research these characteristics,precise orientation of the NV axis in the lattice is essential.Here we show that the orientation of axes of two nearby NV in diamond can be efficiently measured through two beams of polarized light.\end{abstract}\section{text}The measurement of physical quantities is not only a main target but also an active impulsion for scientific research. Especially, it is important to image of nearby particles for modern science[1,2].The accuracy with which two nearby particles can beresolved is classically restricted because of the optical diffraction limit[3].During the last decade, the optical diffraction limit has been overcome with the introduction of several new concepts, pioneered by stimulated emission depletion[4], ground-state depletion[5], structured illumination microscopy[6,7],and image interference microscopy[8].Very recently, imaging methods that used distinguishing information based on photons emitted from different particles have been proposed to achieve precision beyond the diffraction limit. Phenomena from quantum mechanics have been applied to enhance the measurement and have been used to enhance the precision of measurement beyond the classical limit[9,10].So far, in quantum imaging sub-classical resolution has been achieved by using sources of entangled photons[11,13].They are fragile on account of quantum decoherence[14-16].The sub-P0issonian and temporal fluctuation have been applied to enhance the imaging resolution by N with an N th-order process. Until now, a quantum measurement method based on the quantum nature of antibunching photon emission had been developed to detect single particles without the restriction of the diffraction limit. Simultaneously, by counting the single-photon and two-photon signals with fluorescence microscopy, the images of nearby nitrogen-vacancy centers in diamond at distance of 4.25.8±nm had been successfully reconstructed [17]. In addition to imaging nearby NVS, the orientation of the axes of the NVCs is also very important. It is NV that is one of the most intensively studied atom-like solid-state systems in diamond.The NV center is a color defect in diamond consisting of a substituted nitrogen atom associated with an adjacent vacancy(Fig.1). Owing to υ3C symmetry, the NV defect can occur with fourdifferent orientations in the diamond matrix, along ]111[,]111[, ]111[, or ]111[crystallographic axes (Fig.1). In most diamond samples, the NV centers occupy these four orientations equally. The precision of measurement of axes of NV is important for various applications, including the development of hybrid quantum systems, where superconducting qubits are coupled to ensembles of NV defects [18, 19], high sensitivity magnetometry[20-22], and efficient coupling of NV defects to photonic waveguides or microcavities[23-25].For single NV centers, the method of determining the orientation of the NV axis had been published [26].However, there are many combinations of polarization for highly coincident two NVCs. Here, we use two beams of polarized light to measure the axes of highly coincident two NVCs.For this crystal orientation(see Fig.1), from four possible NV orientations, one of them ([111]) is normal to the sample surface. For the other orientations, they are located in the bottom of the directions.The spontaneous emission rates vary with the polarization of the pump beam according to different axes of NVCs and the luminescence intensities for the light polarized parallel (x I ) and perpendicular (y I ) to the laser polarization are [26]:% MathType!MTEF!2!1!+-%feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn %hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr %4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamysamaaBa %aaleaacaWG4baabeaakiabg2da9maalaaabaGaaGymaaqaaiaaikd a% aaGaamyqamaaBaaaleaacaWGWbaabeaakiaacUfaciGGZbGaaiyA ai%aac6gadaahaaWcbeqaaiaaikdaaaGccaGGOaGaeqy1dyMaaiykaia b% gUcaRmaalaaabaGaaGymaaqaaiaaiMdaaaGaci4yaiaac+gacaGGZ b% WaaWbaaSqabeaacaaIYaaaaOGaaiikaiabew9aMjaacMcacaGGDb aa% aa!4E79!${I_x} = \frac{1}{2}{A_p}[{\sin ^2}(\phi ) + \frac{1}{9}{\cos ^2}(\phi )]$% MathType!MTEF!2!1!+-%feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn %hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr %4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9 % vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamysamaaBa %aaleaacaWG5baabeaakiabg2da9maalaaabaGaaGymaaqaaiaaikd a% aaGaamyqamaaBaaaleaacaWGWbaabeaakiaacUfaciGGJbGaai4B ai% aacohadaahaaWcbeqaaiaaikdaaaGccaGGOaGaeqy1dyMaaiykaia b% gUcaRmaalaaabaGaaGymaaqaaiaaiMdaaaGaci4CaiaacMgacaGG Ub% WaaWbaaSqabeaacaaIYaaaaOGaaiikaiabew9aMjaacMcacaGGDb aa% aa!4E7A!${I_y} = \frac{1}{2}{A_p}[{\cos ^2}(\phi ) + \frac{1}{9}{\sin ^2}(\phi )]$Where ? is angle between laser polarization and the projection of each NV axis ,p A is the total spontaneous emission rate.The photoluminescence minima occur when the projection of the NV axis onto the sample surface is parallel to the electric field of the optical excitation. With polarized optical pump for NV, the number of possible orientations of a given center is reduced from four to two, which are in the plane of ?=0?or ?=90?, as shown in Fig.1(b)(再添加进去投影图).With polarized optical pump for the NV toward one side, there will have intensity distribution of two kinds of shapes because of four orientations of axes of NV only have two kinds of polarization, as shown in Fig. 2. Next, we polarized optical pump for the NV toward other side and will get anotherset of intensity distribution. We only conserve ? from ?0to ?180. It have beenknown that intensity has the maximum when ? is ?90. We discuss four caseswhere the nitrogen atoms are likely to be located. We chose three edges to give the excitation light and the relationship between light intensity and angle is shown in Fig.4. (图4还未列出) Last, we simulated the intensity of the three experiments, it includes 6 combinations of possible axial direction for two nearby NVCs. We set that the first time to be excited is the edge of the number 1. From top to down in a counter clockwise direction, we excite the other two edges. (图5) Figure 5 shows the intensity that may appear after three experiments. If it occurs one of four kinds of condition in B, C, D, and E, we just need to excite two times. If the first two times the intensity is not distinguishable just as A and F, we need to excite third times.In summary, we proposed and demonstrated a measurement of axes of two nearby NVCs by spontaneous emission rates vary with the polarization of the pump beam. The orientation of crystallographic axes of two well-overlapping NVCs can be spatially resolved. This work is a significant step towards precision of physical characteristics of the NV for quantum information and sensing applications.[1] P. Alivisatos, Nat. Biotechnol. 22, 47 (2004).[2] G. Patterson, M. Davidson, S. Manley, and J. Lippincott-Schwartz, Annu. Rev. Phys. Chem. 61, 345 (2010).[3]Abbe E (1873) Conributions to the theory of the microscope and the microscopic perception (translated from German). Arch MikrAnat9:413–468.[4] Hell SW, Wichmann J (1994) Breaking the diffraction resolution limit by stimulated emission:Stimulated-emission-depletion fluorescence microscopy. OptLett19:780–782.[5] Hell SW, Kroug M (1995) Ground-state-depletion fluorescence microscopy: A concept for breaking the diffraction resolution limit. ApplPhys B Lasers Optics 60:495–497.[6] Gustafsson MGL (2000) Surpassing the lateral resolution limit by a factor of two using structuredillumination microscopy. J Microsc198:82–87.[7] Heintzmann R, Jovin TM, Cremer C (2002) Saturated patterned excitation microscopy: A concept for optical resolution improvement. J Opt Soc Am A 19:1599–1609.[8] Gustafsson MGL, Agard DA, Sedat JW (1999) (IM)-M-5: 3D wide-field light microscopy with better than100-nm axial resolution.J Microsc Oxford 195:10–16.[9] V. Giovannetti, S. Lloyd, and L. Maccone, Science 306,1330 (2004).[10] LIGO Scientific Collaboration, Nat. Phys. 7, 962 (2011).[11] M. D’Ang elo, C. V. Chekhova, Y. Shih, Phys. Rev. Lett.87, 013602 (2001).[12] P. R. Hemmer et al., Phys. Rev. Lett. 96, 163603 (2006).[13] A. Muthukrishnan, M. O. Scully, M. S. Zubairy, J. Opt. B 6,S575 (2004).[14] T. Nagata, R. Okamoto, J. L. O’Brien, K. Sasak i, and S. Takeuchi, Science 316, 726 (2007).[15] F.W. Sun, B. H. Liu, Y. X. Gong, Y. F. Huang, Z.Y. Ou, and G.C. Guo, Europhys. Lett.82, 24 (2008).[16] G.Y. Xiang, B. L. D. Higgins, W. H. Berry, M.G. Wiseman, and J. Pryde, Nat. Photonics 5, 43 (2011).[17] Jin-Ming Cui, Fang-Wen Sun, Xiang-Dong Chen, Zhao-Jun Gong, and Guang-Can Guo, Phys. Rev. L 110,153901(2013).[18] Y. Kubo, C. Grezes, A. Dewes, T. Umeda, J. Isoya, H. Sumiya, N.Morishita, H. Abe, S. Onoda, T. Ohshimaet al., Phys. Rev. Lett. 107, 220501 (2011).[19] X. Zhu, S. Saito, A. Kemp, K. Kakuyanagi, S. Karimoto, H. Nakano, W. J. Munro, Y. Tokura, M. S. Everitt,K. Nemoto et al., Nature 478, 221 (2011).[20] V. M. Acosta, E. Bauch, M. P. Ledbetter, C. Santori, K.-M.C. Fu, P. E. Barclay, R. G. Beausoleil, H. Linget,J. F. Roch, F. Treussart et al., Phys.Rev. B 80, 115202 (2009).[21] D. Le Sage, K. Arai, D. R. Glenn, S. J. DeVience, L. M. Pham, L. Rahn-Lee, M. D. Lukin, A. Yacoby, A.Komeili, and R. L. Walsworth, Nature 496, 486 (2013).[22] Y. Dumeige, M. Chipaux, V. Jacques, F. Treussart, J.-F. Roch, T. Debuisschert, V. M. Acosta, A. Jarmola, K.Jensen, P. Kehayias et al., Phys. Rev. B 87, 155202 (2013).[23] A. Faraon, P. E. Barclay, C. Santori, K.-M. C. Fu, and R. G. Beausoleil, Nat. Photonics 5, 301 (2011).[24] J. Riedrich-M€oller, L. Kipfstuhl, C. Hepp, E. Neu, C. Pauly,F. M€ucklich, A. Baur, M. Wandt, S. Wolff,M. Fischer et al., Nat. Nanotechnol. 7, 69 (2011).[25] M. Loncar and A. Faraon, MRS Bull. 38, 144 (2013).[26] Thiago P. Mayer Alegre,Charles Santori,Gilberto Medeiros-Ribeiro,and Raymond G. Beausoleil,Phys. Rev. B 76, 165205 (2007)....\end{document}形成的PDF效果图:。
(完整版)latex初学者模板

% a4paper - A4纸11pt -字体 twoside -双面 openany -新章节可在偶数页开始\documentclass[a4paper,11pt,twoside,openany]{article}%------------------------------纸张大小----------------------------------% 定义转换成pdf文档的纸张大小,应与\paperwidth \paperheight一致%\special{pdf: pagesize width 20cm height 30cm}% true的含义是保持尺寸不会随一些参数的变化而变化,具体可见Knuth的TeXbook%\paperwidth 20 true cm % 纸张宽%\paperheight 30 true cm % 纸张高%------------------------------页面布局----------------------------------%\textwidth 10 true cm % 正文宽%\textheight 20 true cm % 正文高%\headheight 14pt % 页眉高%\headsep 16pt % 页眉距离%\footskip 27pt % 页脚距离%\marginparsep 10pt % 边注区距离%\marginparwidth 100pt % 边注区宽%----------------------------页边空白调整-------------------------------\def\marginset#1#2{ % 页边设置\marginset{left}{top}\setlength{\oddsidemargin}{#1} % 左边(书内侧)装订预留空白距离\iffalse % 如果考虑左侧(书内侧)的边注区则改为\iftrue\reversemarginpar\addtolength{\oddsidemargin}{\marginparsep}\addtolength{\oddsidemargin}{\marginparwidth}\fi\setlength{\evensidemargin}{0mm} % 置0\iffalse % 如果考虑右侧(书外侧)的边注区则改为\iftrue\addtolength{\evensidemargin}{\marginparsep}\addtolength{\evensidemargin}{\marginparwidth}\fi% \paperwidth = h + \oddsidemargin+\textwidth+\evensidemargin + h\setlength{\hoffset}{\paperwidth}\addtolength{\hoffset}{-\oddsidemargin}\addtolength{\hoffset}{-\textwidth}\addtolength{\hoffset}{-\evensidemargin}\setlength{\hoffset}{0.5\hoffset}\addtolength{\hoffset}{-1in} % h = \hoffset + 1in\setlength{\voffset}{-1in} % 0 = \voffset + 1in\setlength{\topmargin}{\paperheight}\addtolength{\topmargin}{-\headheight}\addtolength{\topmargin}{-\headsep}\addtolength{\topmargin}{-\textheight}\addtolength{\topmargin}{-\footskip}\addtolength{\topmargin}{#2} % 上边预留装订空白距离\setlength{\topmargin}{0.5\topmargin}}% 调整页边空白使内容居中,两参数分别为纸的左边和上边预留装订空白距离\marginset{10mm}{12mm}%-----------------------------字体支持-----------------------------------\usepackage{times} % 使用 Times New Roman 字体\usepackage{CJK,CJKnumb,CJKulem} % 中文支持宏包%\usepackage{ccmap} % 使pdfLatex生成的文件支持复制等%\usepackage[mtbold,mtpluscal,mtplusscr]{mathtime}%数学环境用Times New Roman%-----------------------------页眉页脚-----------------------------------\usepackage{fancyhdr} % 页眉页脚相关宏包\pagestyle{fancy} % 页眉页脚风格%-----------------------------段落字体格式-------------------------------\usepackage{color} % 支持彩色\usepackage{indentfirst} % 首行缩进宏包%\setlength{\parindent}{2em} % 段落缩进\setlength{\parskip}{0.7ex plus0.3ex minus0.3ex} % 段落间距%\linespread{1.2} % 行距倍数\renewcommand{\baselinestretch}{1.2} % 行距倍数(同上)%\renewcommand{\CJKglue}{\hskip 0pt plus 0.08\baselineskip} % 汉字字距%\newcommand{\aaa}{这是测试} % 自定义文字块例子\newcommand{\song}{\CJKfamily{song}} % 宋体\newcommand{\hei}{\CJKfamily{hei}} % 黑体\newcommand{\fs}{\CJKfamily{fs}} % 仿宋\newcommand{\kai}{\CJKfamily{kai}} % 楷体\newcommand{\li}{\CJKfamily{li}} % 隶书\newcommand{\you}{\CJKfamily{you}} % 幼圆\newcommand{\wuhao}{\fontsize{10.5pt}{12.6pt}\selectfont} % 五号字体\newcommand{\xiaosi}{\fontsize{12pt}{14pt}\selectfont} % 小四字体\newcommand{\sihao}{\fontsize{14pt}{\baselineskip}\selectfont} % 四号字体%\marginparpush %%-----------------------------超链接和标签-------------------------------\iffalse % 将这里改为\iftrue即可使用\ifx\pdfoutput\undefined % Not run pdftex% \ifx% \usepackage[dvips]{hyperref}% \else\usepackage[dvipdfm]{hyperref}% \fi\AtBeginDvi{\special{pdf:tounicode GBK-EUC-UCS2}} % GBK -> Unicode\else\usepackage[pdftex]{hyperref}\fi\hypersetup{CJKbookmarks,%bookmarksnumbered,%colorlinks,%linkcolor=blue,%citecolor=blue,%hyperindex,%plainpages=false,%pdfstartview=FitH}\fi%--------------------------------注释------------------------------------\iffalse % 将这里改为\iftrue即可使用%注释掉一段内容\usepackage{verbatim}\begin{comment}This is a comment example.\end{comment}\fi%\makeatletter % @ is now a normal "letter" for Tex%\makeatother % @ is restored as a "non-letter" for Tex%--------------------------------其他宏包--------------------------------%\usepackage{amsmath,amsthm,amsfonts,amssymb,bm} % 数学宏包%\usepackage{graphicx,psfrag} % 图形宏包%\usepackage{makeidx} % 建立索引宏包%\usepackage{listings} % 源代码宏包%---------------------------------正文-----------------------------------\begin{document} % 开始正文% song-宋体 hei-黑体 fs-仿宋 kai-楷体 li-隶书 you-幼圆 com为 song+hei\begin{CJK*}{GBK}{com} % 开始中文环境\CJKtilde % 重定义~代表的空白距离\CJKindent % 段首缩进\CJKcaption{GB} % 中文章节标题\author{ceo} % 作者\title{一个latex例子} % 题目\maketitle % 生成标题%\thispagestyle{empty} % 设置首页的页眉页脚风格%\setlength{\baselineskip}{3ex plus1ex minus1ex} % 调整行距\TeX{}~是由图灵奖得主\index{Knuth, Donald E.}~Donald E. Knuth\cite{texbook}~编写的计算机程序,用于文章和数学公式的排版。
2024版latexPPT模板[1]
![2024版latexPPT模板[1]](https://img.taocdn.com/s3/m/653fe807777f5acfa1c7aa00b52acfc789eb9f22.png)
01引言Chapter目的和背景目的背景适用范围和使用方法适用范围使用方法02 LaTeXChapterLaTeX概述LaTeX安装与配置编辑器选择及使用技巧03PPT制作要素与规范Chapter01020304统一使用相同的字体、字号、行间距等排版元素,确保整体风格一致。
保持一致性避免过多的文字和图片,突出关键信息,保持页面整洁。
简洁明了通过标题、副标题、正文等层次结构,使内容条理清晰,易于理解。
层次感合理安排页面元素的位置和大小,保持页面平衡和谐。
对齐与平衡页面布局与排版原则色彩搭配与视觉效果提升色彩选择对比度背景与前景图片与图标01020304图表类型选择简洁明了数据准确性数据可视化技巧图表制作及数据可视化方法04 LaTeXChapter主题突出背景简洁Logo 和标题030201封面设计目录结构设置层次分明导航清晰链接跳转正文内容编排技巧图文并茂文字简练结合图片、图表等可视化元素展示数据和信息,提高观众理解度。
突出重点图表插入与编辑方法选择合适图表类型根据数据特点选择合适的图表类型,如柱状图、折线图、饼图等。
数据编辑与格式化在LaTeX中编辑数据,设置图表标题、坐标轴标签等,使图表更加直观易懂。
图表美化调整图表颜色、线条粗细等样式,提升图表美观度。
05常见问题解决方案及优化建议Chapter编译错误处理策略确保LaTeX代码语法正确,特别是命令、环境、括号等。
编译错误时,查看LaTeX编译器提供的错误提示信息,定位问题所在。
将代码分块,逐步排查问题,缩小错误范围。
利用在线LaTeX编辑器或排错工具,检查并修正代码错误。
检查语法错误查看错误提示逐步排查使用在线工具保持一致性在整篇文档中保持字体、字号的一致性,避免过多的样式变化。
字体选择使用`usepackage{fontspec}`命令加载字体包,通过`setmainfont{FontName}`设置主字体。
字号调整使用`fontsize{size}{baselineskip}`命令设置字号和行间距,其中`size`为字号大小,`baselineskip`为行间距。
开题答辩演示文档-latex论文模板

LATEX 与 CLI 绘图工具结合,绘制高精度的图片
expert
update model
initialize model
identify candidate
models
evaluate candidate
models
is best
yes
candidate
better?
no stop
system
LATEX 模板的作用
SCNU LATEX Thesis
Template
Joseph Pan
为什么要推荐 LATEX ?
学位论文的普遍问题 LATEX 简介及特性
研究意义
研究目标
预期成果
技术方案
形式结构 关键设计 成员分工
课题自评
1 提高排版效率,让用户更专注于内容 2 形式与内容分离,安全可靠 3 易于扩展,以适应日后的需求
为什么要推荐 LATEX ?
学位论文的普遍问题 LATEX 简介及特性
研究意义
研究目标
预期成果
技术方案
形式结构 关键设计 成员分工
课题自评
Figure 4: LATEX 与 Word 时间与精力耗费曲线
Joseph Pan (SCNU)
SCNU LATEX Thesis Template
10/11 2011 8 / 17
Template
Joseph Pan
为什么要推荐 LATEX ?
学位论文的普遍问题 LATEX 简介及特性
研究意义
研究目标
预期成果
技术方案
形式结构 关键设计 成员分工
课题自评
1 提高排版效率,让用户更专注于内容 2 形式与内容分离,安全可靠 3 易于扩展,以适应日后的需求
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\end{frame}
\end{CJK*} \end{document}
% 如果你想插入学校的徽章, 其文件名为 "university-logo-filename.xxx", % 其中 xxx 是 pdflatex 能接受的格式, 则可用以下命令插入 % \pgfdeclareimage[height=0.5cm]{university-logo}{university-logo-filename} % \logo{\pgfuseimage{university-logo}}
\usepackage{CJK} % 如果内容中用到定理环境, 则需插入以下命令 %\begin{CJK*}{GBK}{kai} %\newtheorem{thm}[theorem]{定理} %\end{CJK*}
\begin{document}
\begin{CJK*}{GBK}{kai} \CJKtilde \title[短标题]{论文的正式标题} % 如果标题不长, [短标题]可以略去 \s title {也许有的副标题} \author[作者甲等] % (如果作者不多, 则可略去此方括号) {作者甲\inst{1} \and 作者乙\inst{2}} % \inst{?} 仅用于有多个单位的情形 \institute[某甲和某乙大学] % (方括号内的简称是可以略去的) {
\inst{1}% 某甲大学\\ 数学系 \and \inst{2}% 某乙大学\\ 计算机科学系} % \inst 仅用于有多个单位的情形
\date[CFP 2003] % (方括号内的会议简称是可以略去的) {奇妙问题探讨大会, 2003} % 可以使用会议的全称或简称
\s ject{虚拟数学} % 此部分并不重要, 可以省略
\beamertemplatearticlebibitems % 辅以有趣的文章, 越少越好.
\bibitem{Someone2000} 王某某. \newblock 关于这个或那个. \newblock {\em 某某期刊}, 2(1):50--100, 2000.
\end{thebibliography}
\end{frame}
% 以下的演示文稿仅供参考, 不过可以提供一些忠告: % - 除总结外, 最好不超过 3 节; % - 每节至多分成 3 小节; % - 每屏约 30 秒至 2 分钟, 因此总共 15 至 30 屏为佳. % - 一般说来, 会议听众对你所报告的东西知之甚少, 因此尽量简单! % - 在 20 分钟报告里只要讲清主要思想即可, 不要深入细节, 宁可牺牲一点严格性; % - 如果你略去了证明或实现的关键细节, 只要声明一下即可, 没有人会感到不高兴.
第一项. \item<4->
第二项. \end{itemize} \item 使用一般的~\texttt{uncover}~命令: \begin{itemize}
\uncover<5->{\item 第一项.}
\uncover<6->{\item 第二项.}
\end{itemize} \end{itemize} \end{frame}
\begin{frame} \frametitle{使标题富有启发性} 你可以用以下方式创建覆盖片\dots \begin{itemize} \item 利用~\texttt{pause}~命令: \begin{itemize} \item 第一项. \pause \item 第二项. \end{itemize} \item 利用覆盖的明细表: \begin{itemize} \item<3->
\end{frame}
\begin{frame} \frametitle{标题七} 内容七
\end{frame}
\begin{frame} \frametitle{标题八} 内容八
\end{frame}
\section*{总结} \begin{frame}
\frametitle<presentation>{总结} % 是总结保持简短. \begin{itemize} \item
% 如果你想要在每一小节之前都显示一下目录, 则可把一下小段的注解号 "%" 删去 %\AtBeginS section[] %{ % \begin{frame}<beamer> % \frametitle{概要} % \tableofcontents[currentsection,currents section] % \end{frame} %}
\section{动机} \s section{我们研究的基本问题}
\begin{frame} \frametitle{使标题富有启发性} \frames
title{副题是可选的}
\begin{itemize} \item
多使用罗列~(\texttt{itemize})~环境. \item
使用短句. \end{itemize} \end{frame}
% 除掉以下命令的注解 "%" 后, 许多环境都会自动逐段显示 %\beamerdefaultoverlayspecification{<+->}
\begin{frame} \titlepage
\end{frame}
\begin{frame} \frametitle{概述} \tableofcontents % 你也可以插入选项 [pausesections]
% 《LATEX入门与提高》上的一个beamer模板,linux下GBK改为UTF8。
% 20分钟大会报告.tex % 根据 conference-ornate-20min.en.tex,v 1.6 2004/10/07 20:53:08 tantau Exp 改编
\documentclass[cjk]{beamer}
\end{frame}
\begin{frame} \frametitle{标题四} 内容四
\end{frame}
\begin{frame} \frametitle{标题五} 内容五
\end{frame}
\s
section{证明或实现的基本思路}
\begin{frame} \frametitle{标题六} 内容六
以一两行的篇幅列出你的报告的\alert{最主要的结论}. \item
以一两行的篇幅列出你的报告的\alert{次要的结论}. \item
也许还有\alert{第三个结论}, 但不能再多. \end{itemize}
% 以下的展望是可选的. \vskip0pt plus.5fill \begin{itemize} \item
\s section{以前的工作}
\begin{frame} \frametitle{标题一} 内容一
\end{frame}
\begin{frame} \frametitle{标题二}
内容二 \end{frame}
\section{我们的结果或贡献}
\s section{主要结果}
\begin{frame} \frametitle{标题三} 内容三
\mode<presentation> {
\usetheme{Warsaw} % 可以改成别的主题 \setbeamercovered{transparent} % 也可删去 }
\setbeamertemplate{captБайду номын сангаасon}[numbered] %beamer默认的图片的caption不带编号
展望 \begin{itemize} \item
你没有解决的一些问题. \item
你没有解决的另一些问题. \end{itemize} \end{itemize} \end{frame}
% 以下内容是备选的, 一般并不需要. \appendix
\section<presentation>*{附录} \s section<presentation>*{进一步阅读}
\begin{frame}[allowframebreaks] \frametitle<presentation>{进一步阅读} \begin{thebibliography}{10} \beamertemplatebookbibitems % 以综述性书籍当头. \bibitem{Author1990} 张某某. \newblock {\em 关于任何事物的手册}. \newblock 某某出版社, 1990.