摘要
湖南郴州万华岩溶洞是湘南地区最著名的旅游胜地之一,是仍在发育中的大型地下河溶洞系统。万华岩溶洞中“石蛋生笋”奇观更是世界上首次发现,具有不可估量的岩溶科研、旅游观光、洞穴探险价值,但其成因一直不被公众所熟知。本文从地质运动的角度,系统地分析了“石蛋生笋”的成因,其地质形成过程最可能是:岩浆侵入-风化侵蚀-流水搬运-碳酸钙沉积。
Wanhuayan cave in Chenzhou city of Hunan province is one of the most famous tourist attractions in southern Hunan province.It is still a large developing underground river cave system.Wanhuayan karst cave is the first place in the world to discover the “stone eggs give birth to stalagmites”,which has inestimable value for karst scientific research,tourism and spelunking,but its cause has not been well known to the public.From the perspective of geology movements,this paper systematically analyzes the causes of the formation of “stone eggs give birth to stalagmites”.The geological formation process is most likely magma intrusion-weathering and erosion-water transportation-calcium carbonate deposition.
作者
王喆
卢丽
夏日元
曹建文
赵良杰
WANG Zhe;LU Li;XIA Riyuan;CAO Jianwen;ZHAO Liangjie(Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics,MNR&GZAR,Guilin 541004,China)
出处
《中国矿业》
北大核心
2019年第A01期361-362,365,共3页
China Mining Magazine
基金
国家自然科学基金项目资助(编号:41807218
41602277)
中国地质调查局地质调查项目资助(编号:DD20190342
DD20160300)
国家重点研发计划项目资助(编号:2018YFC0604301
2017YFC0406104)
关键词
万华岩溶洞
石蛋生笋
花岗岩
石灰岩
Wanhuayan cave
stone eggs give birth to stalagmites
granite
limestone