1) 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。
2) 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。
3) Maokou(and/or Gufeng) Formation
茅口(孤峰)组
4) the Gufeng formation of Permian
二叠纪孤峰组
5) outlier
[英]['aut,laiə] [美]['aʊt,laɪɚ]
孤残峰
6) multi peak limit cycle
多峰孤立子
补充资料：孤峰溶蚀平原
孤峰溶蚀平原是指峰林平原进一步发育，峰林不断溶蚀降低，地表夷平，仅有少量山峰存在所形成的平原
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