clastics

1.The clastic nodulus, yield stress and stress-strain relationship of two-phase particle composites can be predicted.

该模型由两个简单模型成，它可以方便地预测不同体积比的两相材料的弹性模量、应力—应变响应。

2.Texture of sedimentary rock: clastic texture and nonclastic texture.

碎屑结构和非碎屑结构。

3.The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.

变形带由成，为一套糜棱岩化火山岩、火山碎屑沉积岩。

4.Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.

在红色碎屑岩建造中有层间氧化带和“泥-砂-泥”结构发育，并有良好的地水承压和循环体制，是寻找可地浸砂岩型铀矿的有利地区。