檢視岩石结构的原始碼

{| class="wikitable" align="right"
|-
| style="background: #FF2400" align= center|  '''<big>岩石结构</big>'''
|-
|<center><img src=https://gimg2.baidu.com/image_search/src=http%3A%2F%2Fup.sc.enterdesk.com%2Fedpic%2Fe5%2F97%2F79%2Fe59779b3071d3fd121ccad6219c27158.jpg&refer=http%3A%2F%2Fup.sc.enterdesk.com&app=2002&size=f9999,10000&q=a80&n=0&g=0n&fmt=auto?sec=1659942504&t=8eceda0b9dca571ae3f2607012f814a0 width="300"></center>
<small>[https://image.baidu.com/search/detail?ct=503316480&z=0&ipn=d&word=%E5%B2%A9%E7%9F%B3%E7%BB%93%E6%9E%84&step_word=&hs=0&pn=20&spn=0&di=7108135681917976577&pi=0&rn=1&tn=baiduimagedetail&is=0%2C0&istype=0&ie=utf-8&oe=utf-8&in=&cl=2&lm=-1&st=undefined&cs=779697874%2C2937889896&os=2318220288%2C734279944&simid=779697874%2C2937889896&adpicid=0&lpn=0&ln=1446&fr=&fmq=1657350509362_R&fm=&ic=undefined&s=undefined&hd=undefined&latest=undefined&copyright=undefined&se=&sme=&tab=0&width=undefined&height=undefined&face=undefined&ist=&jit=&cg=&bdtype=0&oriquery=&objurl=https%3A%2F%2Fgimg2.baidu.com%2Fimage_search%2Fsrc%3Dhttp%3A%2F%2Fup.sc.enterdesk.com%2Fedpic%2Fe5%2F97%2F79%2Fe59779b3071d3fd121ccad6219c27158.jpg%26refer%3Dhttp%3A%2F%2Fup.sc.enterdesk.com%26app%3D2002%26size%3Df9999%2C10000%26q%3Da80%26n%3D0%26g%3D0n%26fmt%3Dauto%3Fsec%3D1659942504%26t%3D8eceda0b9dca571ae3f2607012f814a0&fromurl=ippr_z2C%24qAzdH3FAzdH3F4_z%26e3Bfv_z%26e3Bjgpj61jfh_z%26e3Bv54AzdH3Ff7vwtAzdH3Fdlcm80_z%26e3Bip4s&gsm=15&rpstart=0&rpnum=0&islist=&querylist=&nojc=undefined&dyTabStr=MCwzLDQsNiw1LDIsMSw3LDgsOQ%3D%3D 来自 呢图网 的图片]</small>
|-
| style="background: #FF2400" align= center|  '''<big></big>'''

|-

| align= light|

中文名；岩石结构

外文名；texture of rocks

属    于；岩石

包    括；结晶程度、大小、形态
|}
'''岩石结构'''指组成岩石的物质的结晶程度、矿物[[颗粒]]的大小，矿物的形状以及它们之间的相互关系所表现出来的特征。在岩浆岩中，按岩石的结晶程度可将结构分为全晶质结构、半晶质结构和玻璃质结构三大类；按岩石中矿物颗粒的绝对大小可分出粗粒、中粒、细粒、微粒等级别的[[结构]]；按矿物颗粒的相对大小又可划分等粒结构、不等粒结构和斑状、似斑状结构；按岩石中矿物的自形程度，还可分出自形结构、半自形结构及他形结构。另外，岩石中矿物颗粒间的相互关系也是确定[[岩石]]结构类型的依据。<ref>[https://wenku.so.com/d/a4980b7b49674354a92d3a2bf68bb0b6 岩石的结构和构造],360文库 , 2021年2月4日</ref>