• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 40 Issue 6
Dec.  2021
Turn off MathJax
Article Contents
ZHOU Wenlong,Jean Bottazzi,TAN Ming,et al.Mechanism of Miao Chamber in Ziyun county based on terrestrial laser scanning and structural analysis[J].Carsologica Sinica,2021,40(06):965-976. doi: 10.11932/karst20210606
Citation: ZHOU Wenlong,Jean Bottazzi,TAN Ming,et al.Mechanism of Miao Chamber in Ziyun county based on terrestrial laser scanning and structural analysis[J].Carsologica Sinica,2021,40(06):965-976. doi: 10.11932/karst20210606

Mechanism of Miao Chamber in Ziyun county based on terrestrial laser scanning and structural analysis

doi: 10.11932/karst20210606
Funds:

 42161001

 黔科合基础[2017]1172

 黔教合KY字[2017]025

 黔科院J字[2018]11号

  • Received Date: 2021-04-30
  • Publish Date: 2021-12-25
  • Located in Ziyun county of Guizhou Province, Miao Chamber belongs to the Gebihe(another name Getuhe)underground river cave system. It is the largest chamber in the world as known by volume and surface area, and its planar projected area is second only to Sarawak Chamber in Malaysia. In 2014, for the first time, British researchers conducted the terrestrial laser scanning and collected the entire point cloud of Miao Chamber by using Riegl VZ-400 3D laser scanner. Combining the point cloud with the analysis of the geological structure, researchers have obtained the following new understanding of the basic morphological characteristics and control factors of Miao Chamber, (1) The integrity structure of Miao Chamber consists of two chambers and a section of large gallery, and this arched gallery probably becomes the world's largest span cave gallery currently registered. Morphologically, two domes connect with one vault, which shapes like the Chinese character "concave". The upper layer plan view of Miao Chamber presents a double-dome structure with two nearly regular polygons and their pedestals in parallel connection. These two polygons are independent but connect with each other. (2) The polygons of upper Miao Chamber are caused by the dislocation of multiple geological structures. This dislocation produced a set of fracture and joint systems in different directions and grades, and formed a pattern with lattice structure in this region, and then the dense fissures converged in Miao Chamber, which makes the dissolution the most developed. (3) Miao Chamber developed in the core of Jiaoma syncline with thick-massive limestone belonging to lower Permian stratum. The opening fissure at the bottom of the syncline provides good structural conditions for the entry of groundwater, which is a key factor that cannot be ignored for the development of Miao Chamber, one of the world’s hugest. (4) The upper layer gallery in Miao Chamber, together with the layered caves in the region, reflects the dual effects of tectonic uplift and river incision in geological history. It is speculated that in the early period many other streams of water from the high place converged in Miao Chamber toerode a huge underground space. Miao Chamber experienced the transition from hyporheic zone to vadose zone, and finally formed the huge cave chamber that accommodates a large number of collapsing boulders  due to stress adjustments. (5) According to the relationship between geomorphic form and geological structure, the development of "double dome" implies that the special geological structure is conducive to the formation of the huge underground caves in pairs, but the exact structure remains to be ascertained.

     

  • ZHOU Wenlong,Jean Bottazzi,TAN Ming,et al.Mechanism of Miao Chamber in Ziyun county based on terrestrial laser scanning and structural analysis[J].Carsologica Sinica,2021,40(06):965-976.
  • loading
  • https://www.nationalgeographic.com/news/2014/9/1409 27-largest-cave-china-exploration-science/.(accessed September 27, 2020)
    http://www.caverbob.com/rooms.htm.(accessed September 27, 2020)
    Klein, Andrew. HIDDEN WORLDS[G]. Science World, 2015, 71 (8): 16-19.
    BarbaryJ P,BottazziJ,CollignonB,et al.Karstologia Mém-oires N°4 Année 1991 GEBIHE 89, Chapitre 2: Le système de la rivière Gebihe (Ziyun, Guizhou) [R]. 1991: 42-54.
    金玉璋.贵州省紫云县发现面积居世界第二位的岩溶厅堂:格必河-苗厅[J].地质科学,1990(2):204.
    http://www.dili360.com/cng/article/p5350c3d7a6c7135.htm.(accessed September 27, 2020)
    https://www.cgs.gov.cn/xwl/ddyw/201603/t20160309_296491.html.(accessed September 27, 2020)
    https://www.nationalgeographic.com/china-caves/supercave-iframe/iframe.html.(accessed September 27, 2020)
    朱学稳.桂林地区灰岩洞穴的溶蚀形态[J].中国岩溶,1982, 1(2):93-103.
    庞丽伟.老黄龙洞洞穴岩石微形态及洞穴发育演化研究[D].昆明:云南大学,2016.
    吴晓章,谢宏全,谷风云,等.利用激光点云数据进行大比例尺地形图测绘的方法[J].测绘通报,2015,(8):90-92.
    周元杰.探寻地下苍穹:世界上容积最大的洞厅:紫云苗厅[J].生态文明新时代,2018(2):41-46.
    MOURETClaude . The Formation of Large Chambers, With Examples from Laos and Other Countries. [C]//13th International Congress of Speleology, 2001: 177-180.
    张英骏.喀斯特地区地下地形向地表地形的转变过程[C]//中国地理学会地貌专业委员会.喀斯特地貌与洞穴研究[M].北京:科学出版社,1990.
    WhiteW B , WhiteE L . Size scales for closed depression landforms: the place of tiankengs[J]. Cave and Karst Science, 2005, 32(2-3): 111-118.
    WalthamTony . The engineering classification of karst with respect to the role and influence of caves[J]. Int. J. Speleol., 2002, 31(1/4): 19-35.
    GilliEric . Big Karst Chambers: Examples, Genesis, Stability[M]. 2021.
    SmartPeter , EavisAndrew , DixonKevin , et al. Geomorphology of the World's Largest Cave Chambers[C]// Asian Transkarst Conference, 2015.
    Jorda BordehoreL. . Stability Assessment of Natural Caves Using Empirical Approaches and Rock Mass Classifications[J]. Rock Mech Rock Eng, 2017(50): 2143-2154.
    张远海,朱德浩.中国大型岩溶洞穴空间分布及演变规律[J].桂林理工大学学报,2012,32(1):20-28.
    陈建庚.探秘“格凸河”溶洞群[J].地球,2006: 25-26.
    陈建庚.格凸河流域喀斯特地貌奇观与旅游开发简介[A]//全国第十一届洞穴大会学术论文集[C].2005: 175-179.
    曹正端,杨瑞东,高军波,等.贵州紫云方解石矿床地球化学特征及成因研究[J].现代地质,2017,31(4):757-767.
    Encyclopedia of Caves (Second Edition)[M]. 2012: 531-538.
    WALTHAMTONY . Mulu-the ultimate in cavernous karst[J]. Blackwell Science Ltd, GEOLOGY TODAY, 1997, 13(6): 216-222.
    GilliesonD. Caves: Processes, Development and Management[M]. Blackwell Publishers, 1996: 81-87.
    李忠权,刘顺.构造地质学[M].北京:地质出版社,2010.
    张成忠,张新,李洪珍,等.贵州紫云—罗甸县丛里地下河岩溶发育特征[J].四川地质学报,2017,37(2):271-274.
    朱学稳,陈伟海,LynchErin .武隆喀斯特及其地壳抬升性质解读[J].中国岩溶,2007,26(2):119-125.
    熊康宁.新构造运动对贵州锥状喀斯特发育的影响[J].贵州地质,1996,13(2):181-186.
    FarrantA R, SmartP L, WhitakerF F, et al. Long-term Quaternary uplift rates inferred from limestone caves in Sarawak, Malaysia[J]. Geology, 1995, 23(4):357-360.
    GoldscheiderNico , DrewDavid . Methods in Karst Hydrogeology[M]. Taylor & Francis Group, London, UK, 2017.
  • 加载中

Catalog

    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

    Article Metrics

    Article views (1483) PDF downloads(77) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return