The polygonal reticulate structure is well developed and wide spread in the Pagoda Formation limestones in the whole Yangtze region.
网纹构造是宝塔组石灰岩地层中非常发育且分布广泛的一种构造形态 ，其成因一直存在争论和疑问。
The polygonal reticulate structure is well developed and wide spread in the Pagoda Formation limestones in the whole Yangtze region.
网纹构造是宝塔组石灰岩地层中非常发育且分布广泛的一种构造形态 ，其成因一直存在争论和疑问。
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