檢視陆源碎屑岩的原始碼

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| style="background: #FF2400" align= center|  '''<big>陆源碎屑岩</big>'''
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中文名称；陆源碎屑岩

常见成分；石英

分类；砾岩，砂岩，粉砂岩，泥质岩

形成原因；由母岩岩体的机械破碎产生
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'''陆源碎屑岩'''是指沉积物来自大陆物理侵蚀作用，经流水、风、[[冰川]]、泥石流、重力流等搬运到沉积盆地沉积成岩。沉积过程受物理的或机械的因素控制，如流体性质 （气体、液体、固体），运动状态 （流动、波浪） 及其强度控制。碎屑岩占[[沉积岩]]总量的3/4以上。<ref>[https://wenku.baidu.com/view/8858d18ff61fb7360a4c651c.html 陆源碎屑岩概述], 360问答, 2020年1月16日</ref>