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Volume 40 Issue 3
Jun.  2021
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Article Navigation >  CARSOLOGICA SINICA  > 2021  >  40(3): 531-538
WU Guangfen, WANG Jiaxue, YANG Li. Study on the developmental characteristics and mechanism of ectopic stone flower at Duoleyuan karst caves in Yunnan[J]. CARSOLOGICA SINICA, 2021, 40(3): 531-538.
Citation: WU Guangfen, WANG Jiaxue, YANG Li. Study on the developmental characteristics and mechanism of ectopic stone flower at Duoleyuan karst caves in Yunnan[J]. CARSOLOGICA SINICA, 2021, 40(3): 531-538.
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Study on the developmental characteristics and mechanism of ectopic stone flower at Duoleyuan karst caves in Yunnan

  • Faculty of Geography， Yunnan Normal University

  • Publish Date: 2021-06-25
    Abstract
  • Stone flowers （calcite flower， aragonite flower and gypsum flower） are a kind of common secondary chemical sediment in karst caves， which widely distribute on the wall of caves， stalactites， stalagmites and the surface of collapse accumulation bodies，and their shape is varied with different causes of formation.The stone flower on the surface of some high-hanging secondary chemical sediments at the Duoleyuan karst caves in Yunnan is found to be an ectopic stone flower. The cause of formation is that ectopic stone flower was formed by the synergistic action of dripping and splashing during the formation of stone pillars， then the ancient river deposits below the stone pillars were eroded and transported， some stone pillars were suspended to form new stalactites or stalactites-like sediment， hence，the stone flower attached to the bottom of stone pillars were relatively raised and exposed. The ectopic stone flower was firstly discovered in Yunnan，which could be used as an important basis for indicating the evolution of micro-geomorphology in karst caves.

     

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    • References(14)
  • [1]
    邵兆刚，孟宪刚，韩建恩，等.四川龙门山构造带活动的钟乳石记录［J］.地球学报，2014，35（1）：25-30.
    [2]
    张结，周忠发，潘艳喜，等.贵州毕节织金洞上覆土壤CO2变化及其对洞穴滴水水化学特征的影响［J］.环境化学，2017，36（10）：2235-2245.
    [3]
    黄保健，李乐乐，李成展，等.贵州金瓜洞云朵石的特征及成因初探［J］.中国矿业，2018，27（S2）：300-303.
    [4]
    Kowalczk A J， Froelich P N. Cave air ventilation and CO2 outgassing by radon-222 modeling： How fast do caves breathe？［J］. Earth and Planetary Science Letters，2010，289（1-2）：210-219.
    [5]
    张美良，朱晓燕，吴夏，等.广西巴马县水晶宫洞穴沉积物特征及其沉积环境［J］.中国岩溶，2013，32（3）：345-357.
    [6]
    Baker A， Wilson R， Fairchild I J， et al. High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and relationship with last millennium climate［J］.Global & Planetary Change，2011，79（3-4）：303-311.
    [7]
    朱学稳.我国灰岩洞穴次生化学沉积物的沉积类型和形态系统［J］.中国地质科学院院报，1987，6（1）：137-142.
    [8]
    吕金波，李铁英，郑明存，等.北京石花洞岩溶学研究进展［J］.城市地质，2014，9（2）：11-17.
    [9]
    林玉石，张顺治，张美良，等.湘西要坝洞沉积堆积特征及形成时代［J］.西北地质，2007，40（3）： 52-61.
    [10]
    张晓曼，王健，郑倩华，等.河北临城崆山白云洞溶洞地貌和沉积特征及其影响因素［J］.古地理学报，2013，15（1）：49-58.
    [11]
    卢耀如.中国岩溶：景观，类型，规律［M］.北京：地质出版社，1986：111.
    [12]
    周乐福.云南土壤分布的特点及地带性规律［J］.山地研究，1983，1（4）：31-38.
    [13]
    章典.洞穴碳酸钙沉积的水运动条件［J］.中国岩溶，1983，2（1）：31-39.
    [14]
    贺卫，李坡.贵州喀斯特洞穴资源特征及开发利用［J］.贵州师范大学学报（自然科学版），2016，34（3）：1-6.
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