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组成,它可以方便地预测不同体积比两相材性模量、应力—应变响应。
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组成,它可以方便地预测不同体积比两相材性模量、应力—应变响应。
Texture of sedimentary rock: clastic texture and nonclastic texture.
碎结构和非碎结构。
The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.
变形带由下石炭干墩组组成,为一套糜棱化火山、火山碎沉积。
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,是寻找可地浸砂型铀矿有利地区。
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