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

便地预测不同体积比
两相材料
弹性模量、应力—应变响应。
分解
,碎屑状
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

便地预测不同体积比
两相材料
弹性模量、应力—应变响应。
Texture of sedimentary rock: clastic texture and nonclastic texture.
碎屑结构和非碎屑结构。
The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.
变形带由下石炭统干墩
成,为一套糜棱岩化火山岩、火山碎屑沉积岩。
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
地下水承压和循环体制,是寻找
地浸砂岩型铀矿
有利地区。
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