1) upper Member of Guanling Formation
关岭组上段
3) Guanling Formation
关岭组
1.
Chirotherium: Fossil Footprints of Primitive Reptiles in the Middle Triassic Guanling Formation, Zhenfeng, Guizhou Province, China;
贵州贞丰中三叠统关岭组中Chirotherium——原始爬行类足迹研究
2.
Luoping biota come from the second member of the Guanling Formation,and the detailed description of the sedimentology from the Daaozi profile of this member shows the lithological changes:from bioturbation limestone to siliceous nodules and belts limestone(calcium turbidite) and further to the dolomite.
罗平生物群产出于关岭组二段,该段大凹子精细剖面细致的沉积学描述记录显示,剖面岩性变化趋势为:从生物扰动灰岩到含硅质结核的条带泥晶灰岩(钙屑浊积岩)向白云岩演化。
5) upper member of Taiyuan Formation
太原组上段
1.
The upper member of Taiyuan Formation in Baiping minefield is composed of three limestone layers(L7,L8 and L9),mudstone and thin coal seams.
白坪井田太原组上段主要由三层灰岩(L7、L8、L9)、泥岩和薄煤层组成,L7灰岩位于该段底部,是一7煤层顶板。
6) upper member of Yuanli Formation
源里组上段
1.
Using the optimal partitioning method and Markov chain analysis method, the author has made a mathematical statistical study on the lithologies of the upper member of Yuanli Formation, Qingbaikou System as well as on 14 elements, including As, Sb, Cu and Pb, obtained from spectral semiquantitative analysis of the systematic samples collected from this member.
本文采用最优分割和马尔柯夫链分析方法 ,对丰城陶沙南部地区青白口纪源里组上段的岩性及其系统样品的光谱半定量分析的As、Sb、Cu、Pb等14种元素进行数理统计 ,探讨其地层划分、对比 ,并对其沉积环境进行分析。
补充资料：东岭关
东岭关是三国时期关云长“过五关斩六将”的第一关，也是关羽出许昌的第一关。东岭关原址位于白沙水库堤体西侧的山岗之上。沿颖河逆流而上，是战国时期许昌通往古都洛阳的故道。1951年修建白沙水库时，原关址建筑物遭到破坏，但关址位置尚存。此关占地面积近2万平方米，正在修建武圣楼、蹦极、码头、天爷庙、花园广场、别墅、水上乐园、观光果园等旅游配套设施。该景点建成后，与周定王墓自然风光旅游区、浅井逍遥观旅游区和白沙水库景区，由彭化省级公路连接，直接同京深与许洛高速公路连接，形成省级旅游环线，具有良好的开发前景。
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