Xi'an Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2025 Vol. 58, No. 1
Article Contents
Article navigation > Northwestern Geology > 2025 > 58(1): 291-299
Next Article Previous Article

CHEN Guangting, ZHANG Jinming, HAO Chenglu, ZHANG Qilong, ZHANG Hailong. 2025. Analysis on the Geomorphic Type Characteristics and Genetic Evolution of Danxia in Tongde Shizang, Qinghai. Northwestern Geology, 58(1): 291-299. doi: 10.12401/j.nwg.2023165
Citation: CHEN Guangting, ZHANG Jinming, HAO Chenglu, ZHANG Qilong, ZHANG Hailong. 2025. Analysis on the Geomorphic Type Characteristics and Genetic Evolution of Danxia in Tongde Shizang, Qinghai. Northwestern Geology, 58(1): 291-299. doi: 10.12401/j.nwg.2023165
shu

Analysis on the Geomorphic Type Characteristics and Genetic Evolution of Danxia in Tongde Shizang, Qinghai

  • Qinghai Insititute of Geological Survey, Qinghai Province Key Laboratory of Geological Processes and Mineral Resources of Northern Qinghai-Tibet Plateau, Xining 810012, Qinghai, China

More Information
Received Date:  13 December 2021
Revised Date:  15 October 2022
Publish Date:  20 February 2025
    Abstract

  • The Danxia landform landscape with the largest contiguous area and typical morphological characteristics in the upper reaches of the Yellow River Basin is developed in Shizang area of Tongde, Qinghai Province. Based on the field investigation and comprehensive analysis, the Shizang Danxia landform was classified according to the individual landform form, including 7 Danxia positive landform and 5 Danxia negative landform, with diverse types and unique landscape. The Shizang Danxia landform in the formation of paleogene Xining group purple thick layer glutenite, affected by geological structure, physical and chemical weathering, erosion, and gravity machinery, such as the inside and outside sales force shape formation, and go through the red layer accumulation, red basin tectonic uplift, danxia landforms of infancy and adolescence formed four evolutionary stages. It is of theoretical and practical significance to further understand the development of Danxia landform in western China, popularize the knowledge of earth science, and protect and utilize the geoscience tourism resources.

    • FullText(HTML)
  • 加载中
    • References
  • [1] 保广普, 刘春娥, 黄广文. 青海丹霞地貌的分布、特征及演化[J]. 西北地质, 2019, 52(3): 199-208 doi: 10.19751/j.cnki.61-1149/p.2019.03.018

    CrossRef Google Scholar

    BAO Guangpu, LIU Chun'e, HUANG Guangwen. Distribution, Characteristics and Evolution of Danxia Landform in Qinghai[J]. Northwestern Geology, 2019, 52(3): 199-208. doi: 10.19751/j.cnki.61-1149/p.2019.03.018

    CrossRef Google Scholar

    [2] 蔡厚维. 青藏高原的现今地壳活动性[J]. 西北地质, 2009, 42(1): 34-42 doi: 10.3969/j.issn.1009-6248.2009.01.002

    CrossRef Google Scholar

    CAI Houwei. Present Crustal Activity Tibetan Plateau[J]. Northwestern Geology, 2009, 42(1): 34-42. doi: 10.3969/j.issn.1009-6248.2009.01.002

    CrossRef Google Scholar

    [3] 郭福生, 陈留勤, 严兆彬, 等. 丹霞地貌定义、分类及丹霞作用研究[J]. 地质学报, 2020, 94(2): 361-374.

    Google Scholar

    GUO Fusheng, CHEN Liuqin, YAN Zhaobin, et al. Definition, classification, and danxianization of Danxia landscapes[J]. Acta Geologica Sinica, 2020, 94(2). 361-374.

    Google Scholar

    [4] 黄进, 陈致均, 齐德利. 中国丹霞地貌分布(上)[J]. 山地学报, 2015, 33(4): 385-396 doi: 10.16089/j.cnki.1008-2786.000049

    CrossRef Google Scholar

    HUANG Jin, CHEN Zhijun, QI Deli. Study on Distribution of Danxia Landform in China(first)[J]. Mountain Research, 2015, 33(4): 385-396. doi: 10.16089/j.cnki.1008-2786.000049

    CrossRef Google Scholar

    [5] 刘星星, 宋磊, 金彦香, 等. 青藏高原全新世风沙活动历史与环境变化[J]. 干旱区资源与环境, 2013, 27(6): 41-47 doi: 10.13448/j.cnki.jalre.2013.06.036

    CrossRef Google Scholar

    LIU Xingxing, SONG Lei, JIN Yanxiang, et al. History of aeolian deposits in Tibetan Plateau and climate change over Holocene[J]. Journal of Arid Land Resources and Environment, 2013, 27(6): 41-47. doi: 10.13448/j.cnki.jalre.2013.06.036

    CrossRef Google Scholar

    [6] 刘志杰, 孙永军. 青藏高原隆升与黄河形成演化[J]. 地理与地理信息科学, 2007, 23(1): 79-82+91 doi: 10.3969/j.issn.1672-0504.2007.01.019

    CrossRef Google Scholar

    LIU Zhijie, SUN Yongjun. Uplift of the Qinghai-Tibet Plateau and Formation, Evolution of the Yellow River[J]. Geography and Geo-Information Science, 2007, 23(1): 79-82+91. doi: 10.3969/j.issn.1672-0504.2007.01.019

    CrossRef Google Scholar

    [7] 彭华. 中国丹霞地貌研究进展[J]. 地理科学, 2000, 20(3): 203-211 doi: 10.3969/j.issn.1000-0690.2000.03.002

    CrossRef Google Scholar

    PENG Hua. A Survey of the Danxia Landform Research in China[J]. Scientia Geographica Sinica, 2000, 20(3): 203-211. doi: 10.3969/j.issn.1000-0690.2000.03.002

    CrossRef Google Scholar

    [8] 彭华. 丹霞地貌分类系统研究[J]. 经济地理, 2002, 22(S1): 28-35

    Google Scholar

    PENG Hua. The Research on Classification System of Danxia Landform[J]. Economic Geography, 2002, 22(S1): 28-35.

    Google Scholar

    [9] 彭华. 丹霞地貌学[M]. 北京: 科学出版社, 2020

    Google Scholar

    PENG Hua. Danxia geomorphology[M]. Beijing: Science Press, 2020.

    Google Scholar

    [10] 祁生胜, 马志康, 安守文, 等. 1∶25万河南蒙古族自治县幅(I47C002004)区域地质调查报告[R]. 青海省地质调查院, 2008

    Google Scholar

    [11] 祁生胜, 李五福, 于文杰, 等. 青海新一轮地质志修编报告[R]. 青海省地质调查院, 2018

    Google Scholar

    [12] 施雅风, 李吉均, 李炳元. 青藏高原晚新生代隆升与环境变化[M]. 广州: 广东科技出版社, 1998

    Google Scholar

    SHI Yafeng, LI Jijun, LI Bingyuan. Uplift and environmental changes of Qinghai-Xizang(Tibetan) plateau in the Late Cenozoic[M]. Guangzhou: Guangdong Science and Technology Press, 1998.

    Google Scholar

    [13] 王国灿, 曹凯, 张克信, 等. 青藏高原新生代构造隆升阶段的时空格局[J]. 中国科学: 地球科学, 2011, 41(3): 332-349

    Google Scholar

    WANG Guocan, CAO Kai, ZHANG Kexin, et al. Spatio-temporal framework of tectonic uplift stages of the Tibetan Plateau in Cenozoic[J]. Science China Earth Sciences, 2011, 41(3): 332-349.

    Google Scholar

    [14] 肖景义, 陈建强, 张璞. 青海地质旅游发展探讨[J]. 西北地质, 2007, 40(3): 111-117 doi: 10.3969/j.issn.1009-6248.2007.03.013

    CrossRef Google Scholar

    XIAO Jingyi, CHEN Jianqiang, ZHANG Pu. Discussion on Development of Geo-tourism in Qinghai Province[J]. Northwestern Geology, 2007, 40(3): 111-117. doi: 10.3969/j.issn.1009-6248.2007.03.013

    CrossRef Google Scholar

    [15] 张克信, 王国灿, 陈奋宁, 等. 青藏高原古近纪—新近纪隆升与沉积盆地分布耦合[J]. 地球科学(中国地质大学学报), 2007, 32(5): 583-597

    Google Scholar

    ZHANG Kexin, WANG Guocan, CHEN Fenning, et al. Coupling between the Uplift of Qinghai-Tibet Plateau and Distribution of Basins of Paleogene-Neogene[J]. Earth Science-Journal of China University of Geosciences, 2007, 32(5): 583-597.

    Google Scholar

    [16] 张克信, 王国灿, 骆满生, 等. 青藏高原新生代构造岩相古地理演化及其对构造隆升的响应[J]. 地球科学(中国地质大学学报), 2010, 35(5): 697-712 doi: 10.3799/dqkx.2010.085

    CrossRef Google Scholar

    ZHANG Kexin, WANG Guocan, LUO Mansheng, et al. Evolution of Tectonic Lithofacies Paleogeography of Cenozoic of Qinghai Tibet Plateau and Its Response to Uplift of the Plateau[J]. Earth Science-Journal of China University of Geosciences, 2010, 35(5): 697-712. doi: 10.3799/dqkx.2010.085

    CrossRef Google Scholar

    [17] 张克信, 王国灿, 洪汉烈, 等. 青藏高原新生代岩石剥露、沉积与气候演化及其对构造隆升的响应[A]. 中国古生物学会学术年会[C], 2011: 232−234

    Google Scholar

    [18] 张克信, 王国灿, 洪汉烈, 等. 青藏高原新生代隆升研究现状[J]. 地质通报, 2013, 32(1): 1-18 doi: 10.3969/j.issn.1671-2552.2013.01.001

    CrossRef Google Scholar

    ZHANG Kexin, WANG Guocan, HONG Hanlie, et al. The study of the Cenozoic uplift in the Tibetan Plateau[J]. Geological Bulletin of China, 2013, 32(1): 1-18. doi: 10.3969/j.issn.1671-2552.2013.01.001

    CrossRef Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(6)

Tables(1)

Export Citation
PDF
XML

Article Metrics

Article views(198) PDF downloads(18) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020