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,它可以方便不同体积比的两相材料的弹性模量、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.
碎屑结和非碎屑结
。
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间氧化带和“泥-砂-泥”结
发育,并有良好的
下
承压和循环体制,是寻找可
浸砂岩型铀矿的有利
区。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The clastic nodulus, yield stress and stress-strain relationship of two-phase particle composites can be predicted.
该模型两个简单模型组成,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.
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.
变形石炭统干墩组组成,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。
声明:以上例句、词性分类均互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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.
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。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The clastic nodulus, yield stress and stress-strain relationship of two-phase particle composites can be predicted.
该由两个简单
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组组成,为一套糜棱化
、
碎屑沉积
。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在红色碎屑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
铀矿的有利地区。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The clastic nodulus, yield stress and stress-strain relationship of two-phase particle composites can be predicted.
该两个简单
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.
变形带下石炭统干墩组组成,为一套糜棱
化火山
、火山碎屑沉积
。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在红色碎屑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
铀矿的有利地区。
声明:以上例句、词性分类均互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
The clastic nodulus, yield stress and stress-strain relationship of two-phase particle composites can be predicted.
该型由两个
型组成,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.
结构和非
结构。
The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.
变形带由下石炭统干墩组组成,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
型铀矿的有利地区。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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.
由下石炭统干墩组组成,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。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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.
变形带由下炭统干墩组组成,为一套糜棱
化火山
、火山碎屑沉积
。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在红色碎屑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
型铀矿的有利地区。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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组组成,为一套糜火山
、火山碎屑沉积
。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在红色碎屑建造中有层间氧
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。
声明:以上例句、词性类均由互联网资源自动生成,部
未经过人工审核,其表达内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。