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、火山碎屑沉
。
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、火山碎屑沉。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
红色碎屑建造中有
间氧化带和“泥-砂-泥”结
，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。
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