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- W3140451750 abstract "Qiyun 山的 Danxia 地形主要在集团企业说出中间的白垩纪系列的 Xiaoyan 组(K_2x~1 ) 的红小粒上被开发，也就是，它主要被三个指责的地区控制 Jingdezhen-Qimen 指责了地区， Jiangwan-Jiekou 有压缩性的指责的地区并且 Kaihua-Chun'an 合拢指责的地区。在白垩纪时期期间，这个区域第一经历了山岳沉淀变得一个大陆人指责了盆，然后有厚 Cretaceousred 沉积在它上积累了。在意外发生的 neotectonism ，这个区域经历了一个高举的过程，它与经历垂直联合开发的过程的 500-600 m.After 的高度使厚白垩纪成为了沉积进一座山，捱过，剥光和交通，象显然微分的捱过和在沙岩和集团企业之间的岩性学和结构影响的剥光一样，宏大 Danxia 美化由山峰森林组成，陡峭的峡谷，洞，方山，建有城堡的山峰，等等形成的天然桥。在 585 m， 400 m 和 150 m 分别地定位的三个刻痕点通常在 neotectonism 期间反映三个统治高举的过程。" @default.
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- W3140451750 date "2006-01-01" @default.
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- W3140451750 title "Danxia landform genesis of the Qiyun Mountain, Anhui Province" @default.
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