[1]姜勇彪,郭福生,陈珊珊,等.江西信江盆地丹霞地貌空间分布及其成因[J].山地学报,2013,(06):731.
　JIANG Yongbiao,GUO Fusheng,CHEN Shanshan.Spatial Distribution and Its Genesis of the Danxia Landforms in Xinjiang Basin, Jiangxi[J].Mountain Research,2013,(06):731.
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江西信江盆地丹霞地貌空间分布及其成因()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2013年06期
页码:
731
栏目:
地质遗址
出版日期:
2013-01-01

文章信息/Info

Title:
Spatial Distribution and Its Genesis of the Danxia Landforms in Xinjiang Basin, Jiangxi
作者:
姜勇彪;郭福生;陈珊珊;
东华理工大学核资源与环境教育部重点实验室，江西　南昌　330013
Author(s):
JIANG Yongbiao;  GUO Fusheng;  CHEN Shanshan
The Key Laboratory of Nuclear Resources and Environment (Ecit), Ministry of Education, Nanchang 330013, Jiangxi,China
关键词:
信江盆地; 丹霞地貌; 分布特征; 形成机制
Keywords:
Xinjiang Basin;  Danxia Landform;  distribution;  formation mechanism
分类号:
P931
文献标志码:
A
摘要:
信江盆地是我国丹霞地貌发育最典型、最集中的红盆之一。由于控制丹霞地貌演化的红层、构造及外动力等成景要素制约,信江盆地内不同部位丹霞地貌经历了不同的演化进程,发育不同的景观组合。信江盆地边缘主要出露茅店组、河口组和莲荷组巨厚层砾岩、含砾砂岩和砂岩,以铁质胶结和少量钙质胶结为主,可溶性成分含量低,这些红层以发育高大的顶斜型峰林型、峰丛型丹霞地貌组合为特征;盆地中部的河口组上部和塘边组地层岩性以含砾砂岩和砂岩为主,并以钙质胶结为主,可溶性成分含量较低,常发育低矮的圆丘状丹霞地貌组合,大型岩洞是其典型的景观类型,过渡地带主要为河口组上部、塘边组和莲荷组下部的砂岩、含砾砂,丹霞地貌只发育于断层或河流发育...
Abstract:
Xinjiang Basin is one of the most typical and concentrated sites of danxia landform distribution in China. Dued to constraints of genesis system including red beds, structures and exogenic geological process that controlled evolution of it, the danxia landforms in different parts of Xinjiang Basin have undergone different evolutionary processes and formed different landscape assembly. In the margins of the basin there are exposed very thick bedded rocks including conglomerate, pebbly sandstone and sandstone of Maodian, Hekou and Lianhe formation, the cements are mainly ferric and a small amount of calcareous and the content of the soluble ingredient is low. There developed high cliffs and the Danxia Landforms are characteristic with hoodoos and peak clusters with a tilted top. In the middle of the basin there are exposed the upper of Hekou formation and Tangbian formation along the banks of Xinjiang River, the rocks are compose of thick or huge thick bedded sandstone and pebbly sandstone with large cross bedding, calcitic cement and the content of the soluble ingredient is low, in where have developed lower cliffs with round tops and the typical landscape were big stone caves along the banks. Between the margin and middle, there exposed mainly sandstone of the upper of Hekou formation, Tangbian and the lower of Lianhe formation that developed mesa, narrow valley, stone cliffs with flat top.

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备注/Memo

备注/Memo:
收稿日期(Received date)：2013-04-19；改回日期(Accepted) : 2013-08-21。
基金项目（Foundation item）：东华理工大学核资源与环境教育部重点实验室项目资助（编号：NRE1214）项目资助。[Supported by project of the Key Laboratory of Nuclear Resources and Environment (Ecit), Ministry of Education (No. NRE1214).]
作者简介（Biography）：姜勇彪（1969-），男，江西玉山人，副教授，博士，主要从事旅游地学和构造地质学教学和研究工作。[Jiang Yongbiao (1969-), man, Yushan County of Jiangxi Province, associate professor, major in teaching and studying on Geotourism and structural geolgy.] E-mail: rbjgeo@163.com
更新日期/Last Update: 1900-01-01