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干旱区地理 ›› 2014, Vol. 37 ›› Issue (3): 419-428.

• 地表过程研究 • 上一篇    下一篇

张掖丹霞暨彩色丘陵地质成因及与南方丹霞地貌之对比

丁宏伟1,2,王世宇3,尹政1,姚兴荣1,冯建宏1,张旭儒1   

  1. (1    甘肃省地矿局水文地质工程地质勘察院, 甘肃    张掖    734000;    2    中国科学院 寒区旱区环境与工程研究所,甘肃    兰州    730000;    3    甘肃省地质矿产勘查开发局, 甘肃    兰州    730000)
  • 收稿日期:2013-07-15 修回日期:2013-09-21 出版日期:2014-05-25
  • 作者简介:丁宏伟(1963-),男,四川南充人,教授级高级工程师,长期在西北地区从事水工环地质勘查研究评价工作.Email:zydhw8029@163.com
  • 基金资助:

    中国科学院内陆河流域生态水文重点实验室开放基金(91125025);甘肃省地矿局科技领军人才创新工作室(2013-04)基金资助

Geologic origins of danxia and colorful hills of Zhangye and comparison with danxia landform in southern China

DING  Hong-wei1,2,WANG  Shi-yu3,YIN  Zheng1,YAO  Xing-rong1,FENG  Jian-hong1,ZHANG  Xu-ru1   

  1. (1   Institute of Hydro-geoloical and Engineering Geology, Gansu Province Bureau of Geology and Mineral Exploitation and Development, Zhangye 734000, Gansu, China;   2   Key Laboratory in Continental River Basin of Ecological Hydrological of Chinese Academy of Sciences, Lanzhou  730000, Gansu, China;   3   Gansu Province Bureau of Geology and Mineral Exploitation and Development, Lanzhou 730000, Gansu, China)
  • Received:2013-07-15 Revised:2013-09-21 Online:2014-05-25

摘要: 利用实际调查测试资料和已有研究成果,在简述丹霞暨彩色丘陵区自然地理条件、地层构造及分布特征的基础上,全面阐述了祁连造山带前古生代、古生代—中生代地质构造发展变化过程。认为丹霞暨彩色丘陵成景地层大约形成于中生代末期100~140 Ma BP前后的早白垩纪,沉积环境为河流-湖泊相红色及杂色层状碎屑岩沉积,总厚度大于5 000 m。以青藏高原隆升为契机,宏观分析了新生代以来喜马拉雅、青藏、昆(仑山)黄(河)、共和四大构造运动及其由此引起的外动力条件的变化对丹霞暨彩色丘陵地貌各个阶段的演化并最终成型的影响和控制。认为喜马拉雅构造运动末期8 Ma BP前后,隆升效应波及到祁连山区,成景地层受到挤压抬升和变形缩短,进而发生轻微褶曲并被长期风蚀、水侵及夷平;6~7 Ma BP上新世,丹霞暨彩色丘陵地貌的雏形基本形成;昆(仑山)黄(河)运动结束后,大约0.2~0.4 Ma BP中更新世,张掖丹霞暨彩色丘陵地貌已完全形成;共和运动期间丹霞暨彩色丘陵地貌区祁连山平均上升幅度为1.32~2.34 mm/a。微观分析了幼年期、中年期、老年期及消亡期丹霞地貌的形成机理和外观特征;从沉积物Fe3+/Fe2+含量及当时环境下的氧化—还原程度诠释了彩色地层的形成原因;从沉积环境、地质构造、地层岩性、地层时代及类型等方面剖析了张掖丹霞暨彩色丘陵与我国南方丹霞地貌的相同与不同之处。

关键词: 丹霞, 彩色丘陵, 地质构造, 成因, 特征, 祁连山

Abstract: This paper introduces the process of development and variation of geologic structure of the Qilian Mountains orogenic belt from the Prepaleozoic era to the Paleozoic era,finally to the Mesozoic era,using practical research results and available research achievements,and based on analyzing the physical geographic condition of danxia landform and colorful hills,geologic structure and distribution characteristics.  From the analyzing the depositional environment,stratum,lithological characteristics,regional structure pattern and forming time,it is believed that the stratum was formed about 100-140 Ma BP,which is during the early cretaceous period. The stratum of total thickness of 5 000 m belongs to river-lacustrine facies red and motley lamellar clastic rock deposition. It is clearly claimed that with the uplift of the Qinghai-Tibet Plateau,rudiment of danxia and colorful hills was nearly formed during 6-7 Ma BP of Pliocene,completely formed during 0.2-0.4 Ma BP of middle Pleistocene.  Besides,according to the internal and external forces of forming the Danxia and colorful hills,the micro analyses were carried out to explore the formation mechanism and appearance features of Danxia landform in the periods of its infancy,middle age,old age and die out age. What’s more,the paper explains the reasons for the sediments forming motley stratum,which is related with the content of Fe3+/Fe2+ and the degree of redox reaction at that time. It is thought that the main color of the stratum is purplish red or brick-red if the stratum has large content of Fe3+ and high ratio of Fe3+/Fe2+,the main color of the stratum is white and black if the stratum has large content of Fe2+ and lower ratio of Fe3+/Fe2+. Furthermore,the article analyses the similarities and differences between Zhangye danxia landform and other danxia landform in southern China,including the depositional environment,geologic structure,stratum lithology and ages and types of stratum and so on. It is believed that Zhangye danxia is an unusual one because it not only has common features of Guangdong danxia landform,which is like the cliffs,but also has common characteristics to Five-color Town in Xinjiang,China,which is colorful. The Zhanye danxia has strong typicality and aesthetic,scientific investigation and ornamental values,which is one of the best seven beautiful danxias in China.

Key words: danxia landform, colorful hills, geologic structure, origins, features, the Qilian Mountains

中图分类号: 

  • P901