1) Hunan and Guizhou
湘黔
1.
Geological Characters and Causation of Multi-element Concentration Stratum of Black Rock Series,Lower Cambrian Series in Hunan and Guizhou
湘黔下寒武统黑色岩系“多元素富集层”地质特征及成因探讨
2) Western Hunan-Eastern Guizhou Province
湘黔区域
5) border of Guizhou and Hunan
湘黔交境
1.
Many newly_discovered paleo_karst unconformity interfaces and exposure zones and some para_sequences and their superimposed patterns can both be employed to divide the Middle-Upper Cambrian dolomite facies in border of Guizhou and Hunan into seven third_order sequences.
根据新发现的许多古岩溶不整合面和暴露带 ,以及副层序和副层序叠置规律 ,将湘黔交境台地中晚寒武世娄山关组 (白云岩相 )划分为 7个三级层序 ,每一层序都由海进体系域和高水位体系域组成 ,缺少低水位体系域沉积 。
6) Guizhou and Hunan regions
湘黔地区
1.
It is obvious that sedimentation responsed to sea level rising during Middle Ordovician in the Guizhou and Hunan regions.
中奥陶世克拉道克阶（Ｃａｒａｄｏｃｉａｎ）在全球范围内为海侵期，体现在全球范围广泛的黑色页岩沉积及笔石动物的大规模繁盛，湘黔地区这一时期地层发育完全，从碳酸盐台地－斜坡－外陆架盆地均有不同程度的响应。
补充资料：湘黔铁路
从湖南株洲经湘潭到贵州贵阳。其中贵定至贵阳段长76千米，与黔桂线合一，1958年筑成。株洲至贵定段长821千米，1972年筑成。是连接中国华中和西南地区的重要通道，与贵昆和浙赣、沪杭等线组成长江以南东西交通大动脉。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条