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吉林省喀斯特洞穴的基础研究 被引量:7

Basic Researches on Karst Caves in Jilin Province
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摘要 论述了吉林省喀斯特洞穴的分布、形成条件、景观特征及其主要形成原因。经野外实地考察发现吉林省共有喀斯特洞穴50余个,它们分布在通化市、白山市及其附近地区,这里碳酸盐岩厚度较大,纯度较高,为洞穴的形成奠定了物质基础。以第三纪为主要发育阶段的古喀斯特洞穴在数量上占明显优势。洞穴属于水平溶洞类型,多数规模较小,但在适宜岩溶发育的地区,也可形成几百米长的大型溶洞。洞内有化学沉积物、崩塌堆积物等,地下河不发育。 t is discussed the distribution,formative condition,landscape characteristics and major formative factor of the karst caves in Jilin province.lt is investigated the karst caves on the spot and found that there are about 50 karst caves in Jilin province, which are distributed in Tonghua City,Baishang City and nearby regions. The carbonate rock with bigger thickness and pureness has laid a material base for the formation of caves.In quantity,the old karst caves occupy a dominant position, which mainly grew in Tertiary period.The karst caves belong to the type of level caves, most of them are small, but in the area suitable to the growth of karst caves,there are large caves of several hundred meters long. In caves there are chemical deposit,collurial deposit and ect. underground streams don't develop.
出处 《东北师大学报(自然科学版)》 CAS CSCD 1995年第3期113-117,共5页 Journal of Northeast Normal University(Natural Science Edition)
关键词 吉林 喀斯特 洞穴 景观特征 洞穴成因 he karst cave in Jilin province landscape characteristics of the cave the formative factor of the cave
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参考文献2

  • 1张普林,吕宝臣,李春田,孙家儒,刘爱.早第三纪桦甸动物群的发现及其地质意义[J]吉林地质,1986(04).
  • 2宋恩宝.通化煤矿区奥陶纪石灰岩岩溶发育规律的探讨[J]吉林地质,1986(01).

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