CAJ | 학술논문

全面介绍北京石花洞发现与研究的历史、取得的重大成果，以及在岩溶学研究领域所起的作用。石花洞位于北京西山，发现于明朝正统十一年，开发于20世纪80年代。岩溶学研究表明，石花洞洞层多（8层），石盾多（200多个），为世界罕见。在全国范围内，首次发现月奶石，首次发现碳酸钙微层理，首次发现膜足硬肢马陆穴居动物。笔者从地质学、气象学和环境学全面研究了石花洞，测绘精度达到1︰200，进行了氡浓度研究。从溶蚀形态来看，石花洞8层溶洞展示北京西山的8次隆升；从沉积形态来看，石花洞中的粗犷石笋代表中更新世沉积，杆状石笋代表晚更新世沉积，微层理石笋代表全球转暖以来的全新世沉积，奠定了首次建立第四纪石笋剖面的基础。
전면개소북경석화동발현여연구적역사、취득적중대성과，이급재암용학연구영역소기적작용。석화동위우북경서산，발현우명조정통십일년，개발우20세기80년대。암용학연구표명，석화동동층다（8층），석순다（200다개），위세계한견。재전국범위내，수차발현월내석，수차발현탄산개미층리，수차발현막족경지마륙혈거동물。필자종지질학、기상학화배경학전면연구료석화동，측회정도체도1︰200，진행료동농도연구。종용식형태래간，석화동8층용동전시북경서산적8차륭승；종침적형태래간，석화동중적조광석순대표중경신세침적，간상석순대표만경신세침적，미층리석순대표전구전난이래적전신세침적，전정료수차건립제사기석순부면적기출。
The paper introduces Shihua Cave’s discovery and study history, as well as great research results and its karst functions. Beijing Shihua Cave, located at Beijing Western Hills, was discovered in the year of 1446 (the 11th year of Zhengtong in Ming Dynasty) and started to develop in the 1980s. Karst research results show that Shihua Cave is rare in the world for multiple layers and cave shields. Furthermore, in Shihua Cave it is the first time in China to discover the moonmilk stone, laminae in stalagmite and diplopoda (Skleroprotopus membranipedalis,sp.nov.). The paper has studied Shihua Cave from geology, meteorology and environmentlogy, radon concentration measurement, and its mapping scale is up to 1:200. In Shihua Cave it has established the foundation for Quaternary stalamite profile-the eight-layer karst caves display eight-phase Neotectonic uplifts of Beijing Western Hills. In the sedimentary view, the wide stalagmites were formed in Middle Pleistocene, rod-like stalagmites were formed in Later Pleistocene, laminae in stalagmite formed in Holocene. the results have got the foundation for establishing the first Quaternary section of stalagmite.