%0 Journal Article
%T Danxia Landform Genesis on Qiyun Mountain, Anhui Province<br>安徽齐云山丹霞地貌成因
%A ZHU Cheng
%A PENG Hua
%A Li Shicheng
%A HUANG Linyan
%A Zheng Chaogui
%A Xiang Fusheng
%A SUN Yufei
%A TANG Yunsong
%A Hu Jiyuan
%A Zhu Guanghui
%A Lu Jianjun
%A Cheng Guanghua
%A <br>朱诚
%A 彭华
%A 李世成
%A 黄林燕
%A 郑朝贵
%A 项伏生
%A 孙毓飞
%A 唐云松
%A 胡济源
%A 朱光辉
%A 吕健君
%A 程光华
%J 地理学报
%D 2005
%I 
%X The Danxia landform of Qiyun Mountain is mainly developed on red sands tone and conglomerate of middle Cretaceous series (K2x1). The landform developme nt in this area is mainly controlled by three faulted zones, that is, Jingdezhen -Qimen faulted zone, Jiangwan-Jiekou faulted zone and Kaihua-Chun'an faulted zon e. During the Cretaceous period, this area firstly experienced massif subsidence to a continental fault basin, and received thick Cretaceous red beds to accumul ation. Then, during neotectonism, this area experienced an uplift process, the t hick Cretaceous sediments became a mountain body with an altitude of 500-600 m. After having undergone the processes of vertical joints development, weathering, denudation and transportation, as well as influenced by the lithological compon ent and structure between the sandstone and the conglomerate, grand Danxia lands cape has formed in this area such as peak forest, steep cliff, cave, mesa, caste llated peak and natural bridge. The three-grade knick points of Qiyun Mountain i llustrates that the area has experienced three major uplift processes during the neotectonism.
%K Qiyun Mountain
%K Danxia landform
%K landform genesis<br>齐云山
%K 丹霞地貌
%K 地貌成因
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=869B153A4C6B5B85&jid=F7B5B947C24B9D649491012214E4BEF4&aid=855B4D9C86BBE3CE&yid=2DD7160C83D0ACED&vid=BFE7933E5EEA150D&iid=38B194292C032A66&sid=A48DE16C07AAAB06&eid=366B1248A15658C5&journal_id=0375-5444&journal_name=地理学报&referenced_num=10&reference_num=31