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

该型由两个简单型组成，它可以方便地预测不同体积比的两相材料的弹性、力—变响。

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.

变形带由下石炭干墩组组成，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.

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

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的两相材料的弹性模量、应力—应变响应。

Texture of sedimentary rock: clastic texture and nonclastic texture.

构和非构。

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，为一套化火山、火山沉积。

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

在红色建造中有层间氧化带和“泥-砂-泥”构发育，并有良好的地下水承压和循环体制，是寻找可地浸砂型铀矿的有利地区。

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，它可以预测不同体积比的两相材料的弹性模量、应力—应变响应。

Texture of sedimentary rock: clastic texture and nonclastic texture.

碎屑和非碎屑。

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“-砂-”发育，并有良好的下水承压和循环体制，是寻找可浸砂岩型铀矿的有利区。

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，它以方便预测不同体积比的两相材料的弹性模量、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.

变形带由下石炭干墩组组成，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，并有良好的下水承压和循环体制，是寻浸砂岩型铀矿的有利区。

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

该由两个简组成，它可以方便预测不同体积比两相材料弹性量、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.

变形带由下石炭干墩组组成，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，并有良下水承压和循环体制，是寻找可浸砂岩铀矿有利区。

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

该模由两个简单模组成，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。

Texture of sedimentary rock: clastic texture and nonclastic texture.

结构和非结构。

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.

在红色建造中有层间氧化带和“泥-砂-泥”结构发育，并有良好的地下水承压和循环体制，是寻找可地浸砂矿的有利地区。

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

由两个简单组成，它可以方便地预测不同体积比的两相材料的弹性量、应力—应变响应。

Texture of sedimentary rock: clastic texture and nonclastic texture.

碎屑结构非碎屑结构。

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

变形带由下石炭干墩组组成，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“泥-砂-泥”结构发育，并有良好的地下水承压体制，是寻找可地浸砂岩铀矿的有利地区。

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

该型由两个简单型组成，它可以方便地预测不同体积比的两相材料的弹性、力—变响。

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.

变形带由下石炭干墩组组成，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.

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

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的两相材料的弹性模量、应力—应响应。

Texture of sedimentary rock: clastic texture and nonclastic texture.

碎屑和非碎屑。

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

形带由下石炭干墩组组成，为棱岩化火山岩、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”发育，并有良好的地下水承压和循环体制，是寻找可地浸砂岩型铀矿的有利地区。

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的两相材料的弹性模量、应力—应变响应。

Texture of sedimentary rock: clastic texture and nonclastic texture.

构和非构。

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，为一套化火山、火山沉积。

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

在红色建造中有层间氧化带和“泥-砂-泥”构发育，并有良好的地下水承压和循环体制，是寻找可地浸砂型铀矿的有利地区。