1) Maokou(and/or Gufeng) Formation
茅口(孤峰)组
2) Gufeng formation
孤峰组
1.
Studies on Radiolarian Fauna from Gufeng Formation in Anhui and Jiangsu Provinces,East China and Its Paleoenviromental Significance;
苏皖地区孤峰组放射虫动物群及其古环境意义
2.
Geochemistry and Origin of Siliceous Rocks from the Gufeng Formation of Middle Permian in the Pingdingshan Area,Chaohu Region,Anhui Province;
安徽巢湖平顶山中二叠统孤峰组硅质岩的地球化学特征及成因
3.
The Tangtian manganese ore deposit lies in Gufeng formation of Permian system in Guichi area, Anhui province including sedimentary carbonatemanganese ore and the oxidized manganese ore.
安徽贵池地区唐田沉积锰矿床赋存于二叠系孤峰组,包括沉积作用形成的碳酸锰矿和经后期氧化作用形成的氧化锰矿,地球化学特征表现为Mn的强烈富集,尤其是氧化锰矿的富集作用更为明显,而Ca,Mg,Si则大量流失,认为锰矿层及含锰岩系的物源既有陆源,又有海源,其沉积水体较深,结合沉积特征及地史演化分析,自栖霞期发生的海侵在茅口早期达最大,矿区处于深水陆棚相-盆地相沉积环境,发生含锰地层的沉积。
3) Kuhfeng Formation
孤峰组
1.
A well preserved Middle Permian radiolarian fauna of the Kuhfeng Formation is for the first time described from Renhua area of Shaoguan, Guangdong Province, South China.
首次描述广东仁化地区中二叠世孤峰组放射虫 Pseudoalbaillella fusiformis- Ps。
2.
The relatively rich radiolarians of the Kuhfeng Formation found from Tianbaoshan in Nanjing,and from Pingdingshan of Chaohu,Yangongtang of Jingxian and Yashan of Nanling in Anhui comprise 14 species and 2 unnamed species,belonging to 7 genera,which are grouped in 6 families and may be divided into 3 radiolarian assemblage zones,namely,the Pseudoalbaillella fusiformis-Ps.
南京天宝山、安徽巢湖平顶山、泾县晏公堂和南陵丫山孤峰组中含有较丰富的放射虫化石，包括７属１６种（未定种），分属于６个科，可以分成三个化石组合带，即下部的Ｐｓｅｕｄｏａｌｂａｉｌｌｅｌｌａｆｕｓｉｆｏｒｍｉｓ－Ｐｓ。
4) Maokou formation
茅口组
1.
Exploration for Natural Gas in Middle Permian Maokou Formation of Sichuan Basin;
四川盆地中二叠统茅口组天然气勘探
2.
Paleokarst unconformity on top of the Maokou Formation in the Jianshi-Badong area, Hubei: its discovery and significance;
湖北建始—巴东地区茅口组顶部古岩溶不整合面的发现
3.
Comprehensive studies have been conducted to investigate sedimentary environment of the Maokou Formation in Huopu section, Panxian, Guizhou province.
根据贵州火铺茅口组剖面的实际材料 ,采用聚类分析等方法对该地茅口组的沉积环境进行了详细研究。
5) limestone of the Maokou Formation
茅口组灰岩
1.
Paleo-karst landforms on top of limestone of the Maokou Formation in the west of the Upper Yangtze platform and its geological significance;
上扬子西部茅口组灰岩顶部古喀斯特地貌的厘定及地质意义
6) the Gufeng formation of Permian
二叠纪孤峰组
补充资料：孤峰塔
孤峰塔坐落在与常德城隔江相望的德山孤峰岭。原孤峰塔始建于明万历三十五年（1607），初名“文峰塔”，与北岸笔架城遥相映衬，象征常德人杰地灵，文运昌盛，后毁于战火。现有的孤峰塔是在原塔基上重建的，塔高33米，底径7米，七级八面，四周八角檐上装有铜铃；塔内有旋梯直到塔顶，游人登塔极目四望，周围的沅江及城市风光尽收眼底。
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