檢視成岩作用的原始碼

[[File:成岩作用.jpg|缩略图|[https://image.baidu.com/search/detail?ct=503316480&z=0&ipn=d&word=%E6%88%90%E5%B2%A9%E4%BD%9C%E7%94%A8&step_word=&hs=0&pn=0&spn=0&di=179630&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=91980898%2C1285201287&os=1520997979%2C4163697271&simid=4217695430%2C715782681&adpicid=0&lpn=0&ln=1482&fr=&fmq=1623297412645_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%2Fimg1.jiemian.com%2Fjiemian%2Foriginal%2F20180628%2F153017858492172600_a580xH.jpg%26refer%3Dhttp%3A%2F%2Fimg1.jiemian.com%26app%3D2002%26size%3Df9999%2C10000%26q%3Da80%26n%3D0%26g%3D0n%26fmt%3Djpeg%3Fsec%3D1625889425%26t%3D5550de7763fca5407028bfe13ed697aa&fromurl=ippr_z2C%24qAzdH3FAzdH3Fooo_z%26e3B3tj4twg_z%26e3Bv54AzdH3Fw6ptvsjAzdH3Fddmbcbb_z%26e3Bip4s&gsm=2&rpstart=0&rpnum=0&islist=&querylist=&nojc=undefined 原图链接][https://www.jiemian.com/article/2268588.html 来自界面新闻]]]
'''成岩作用'''(diagenesis)是指在一定压力、温度的影响下，由松散的沉积物转变为沉积岩的过程。成岩作用多发生在地下几千米以内的地质环境中，成岩作用的主要方式有：压实作用、胶结作用、重结晶作用和新矿物的生长