a clastic anatomical model.
可拆开解剖模型
a clastic anatomical model.
可拆开解剖模型
Texture of sedimentary rock: clastic texture and nonclastic texture.
沉岩结构:碎结构和非碎结构。
Weidongzhuang Formation is of meta-clastics with characteristics of arc-basin clastics.
卫东庄组为一变质碎岩建造,具弧盆碎岩沉特征。
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比两相材料弹性模量、应力—应变响应。
The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.
变形带由统干墩组组成,为一套糜棱岩化火山岩、火山碎沉岩。
The weathering profiles of WC3 and DBK are of clastic rocks, grain size frequency distribution curves of quartz show single, broad peak, and their modes are approximately 5.1φ and 6φ respectively.
两条碎岩风化剖面(WC3和DBK)频率分布曲线呈单峰宽峰态,众数值分别约为5.1φ和6φ。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在红色碎岩建造中有层间氧化带和“泥-砂-泥”结构发育,并有良好地水承压和循环体制,是寻找可地浸砂岩型铀矿有利地区。
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