yuyin
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@ -76,10 +76,10 @@
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<a class="bottomItem" href="./machine.html">
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<img src="./image/2.png" />AI智能服务
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</a>
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<a class="bottomItem" href="javscript:void(0)">
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<a class="bottomItem" href="javscript:void(0)">
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<img src="./image/3.png" />战略目标库
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</a>
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<a class="bottomItem" href="./datail.html">
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<a class="bottomItem" href="./datail.html">
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<img src="./image/4.png" />制式报告输出
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</a>
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</div>
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@ -131,6 +131,11 @@
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function cancelVoice(){
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$(".voicePanel").removeClass("active");
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}
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function sureVoice(){
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$(".voicePanel").removeClass("active");
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$(".fixed-left").addClass("collpased").css({left:"0px"});
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init(name);
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}
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$(function(){
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$(".show_detail").hover(function(){
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$(this).find(".detail_info").show();
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32
datail.html
32
datail.html
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@ -5,22 +5,22 @@
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<title>详细信息</title>
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<link rel="stylesheet" href="./detail.css"/>
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<script src="./js/jQuery-1.8.3.min.js"></script>
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<script src="https://cdn.bootcss.com/html2canvas/0.5.0-beta4/html2canvas.js"></script>
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<script src="./js/html2canvas.js"></script>
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<script src="https://cdn.bootcss.com/jspdf/1.3.4/jspdf.debug.js"></script>
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</head>
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<body>
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<div class="carouselBottom">
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<a class="bottomItem" href="javscript:void(0)">
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<a class="bottomItem" href="javscript:void(0)">
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<img src="./image/1.png">服务优势
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</a>
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<a class="bottomItem" href="./machine.html">
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<a class="bottomItem" href="./machine.html">
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<img src="./image/2.png">AI智能服务
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</a>
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<a class="bottomItem" href="javscript:void(0)">
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<a class="bottomItem" href="javscript:void(0)">
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<img src="./image/3.png">战略目标库
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</a>
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<a class="bottomItem active" href="./datail.html">
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<a class="bottomItem active" href="./datail.html">
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<img src="./image/4.png">制式报告输出
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</a>
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</div>
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@ -93,18 +93,18 @@
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岩石组合为花岗斑岩、花岗闪长岩、闪长玢岩、石英闪长岩、英云闪长岩、二长花岗岩等
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</div>
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<h3>冰川分布</h3>
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<div class="para">
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班公湖为藏北高原西缘东西长约125公里的狭长构造湖,按照国际冰川编目原则,
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<div class="para">
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班公湖为藏北高原西缘东西长约125公里的狭长构造湖,按照国际冰川编目原则,
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班公湖流域区是以该湖为主要流域, 并包括泽普错 、斯潘古尔湖、沙尔达湖和热帮错等若干
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山间小湖群的一个三级流域区整个流域区地理位置介于32°40′~34°30′N和 78°38′~81°15′E之间,
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中国班公湖流域区总共有冰川959条,冰川总面积665.35 平方公里,冰储量为39.2316立方千米,
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昌隆河流域、由昂则、展穷和展金等支流形成的多玛河流域、以及山间湖盆泽普错流域是班公湖
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北岸的冰川主要分布区,南岸流域区冰川则主要分布在由巴扎雄、藏藏布河和曲垄藏布形成的玛
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卡藏布河 、山间小湖盆斯潘古尔湖和沙尔达湖等流域。班公湖流域冰川分别占流域区总数的72.9%、67%
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卡藏布河 、山间小湖盆斯潘古尔湖和沙尔达湖等流域。班公湖流域冰川分别占流域区总数的72.9%、67%
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和64%,流域内冰川平均面积为0.64平方公里,最大的冰川面积23.68平方公里,长度10.5公里,泽普错是
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本流域区中冰川分布最为集中、冰川数量仅次于班公湖的小流域,其冰川数量分别占流域区总数的14.8%、
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28.3%和33.3%,泽普错流域冰川平均面积达1.33平方公里,最大冰川面积16.60平方公里。 [4]
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</div>
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</div>
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<div class="level-2">
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<h2>军事价值</h2>
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</div>
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@ -157,24 +157,24 @@
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$("#pdf,#png").hide();
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makeMpdf();
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setTimeout(()=>{
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$("#pdf,#png").show();
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$("#pdf,#png").show();
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},2000)
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})
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})
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// 导出png
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$("#png").on("click",() => {
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$("#pdf,#png").hide();
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saveCanvas();
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setTimeout(()=>{
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$("#pdf,#png").show();
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$("#pdf,#png").show();
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},2000)
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})
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})
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function makeMpdf () {
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if(confirm("您确认下载该PDF文件吗?")){
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var pdf = new jsPDF('p','pt','a4');
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// 打印比例
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// 打印比例
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pdf.internal.scaleFactor = 2;
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var options = {
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pagesplit: true,
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pagesplit: true,
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"background": '#FFFFFF' // 背景色
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};
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var printHtml = $('.box-con').get(0);
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}
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</script>
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</body>
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</html>
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</html>
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10
detail.css
10
detail.css
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@ -55,9 +55,6 @@ h3{
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font-weight: 400;
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margin-left: 25px;
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}
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.img-con{
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float: right;
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}
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.header{
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clear: both;
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height: 40px;
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@ -71,13 +68,14 @@ h3{
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padding-left: 10px;
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}
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.img-list{
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display: flex;
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height: 120px;
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padding-top: 15px;
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text-align: left;
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}
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.img-list > div{
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margin: auto;
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width: 250px;
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height: 180px;
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float: left;
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}
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.img-list > div>img{
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width: 80%;
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@ -128,4 +126,4 @@ h3{
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font-size: 14px;
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transition: all 0.3s;
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display: none;
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} */
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} */
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