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高校地质学报 ›› 2021, Vol. 27 ›› Issue (4): 480-488.DOI: 10.16108/j.issn1006-7493.2020054

• 其他学科 • 上一篇    下一篇

滇中富民县宝石洞旅游地质特征与成景机制探讨

周余国1,2,张 帆1,2,3*,周 坤4,周琛粟3,王玉朝1,2,王 健1,2,范 凯1   

  1. 1. 云南大学 地球科学学院,昆明 650091; 2. 云南省地理研究所 喀斯特研究与洞穴探测中心,昆明 650091; 3. (香港)中国探险学会,香港 999077; 4. 云南省地质调查局 区域地质调查所,昆明 650200
  • 出版日期:2021-08-20 发布日期:2021-08-30

Discussion on Geological Characteristics and Landscaping Mechanism of Gemstone Cave in Fumin County, Central Yunnan

ZHOU Yuguo1,2,ZHANG Fan1,2,3*,ZHOU Kun4, ZHOU Chensu3,WANG Yuchao1,2,WANG Jian1,2,FAN Kai1#br#   

  1. 1. School of Geoscience, Yunnan University, Kunming 650091, China;
    2. Center of Karst Research and Cave Exploration, Yunnan Institute of Geography, Kunming 650091, China;
    3. (Hong Kong) Chinese Adventure Society, Hong Kong 999077, China;
    4. Institute of Regional Geology Survey,Yunnan Bureau of Geological Survey, Kunming 650200, China
  • Online:2021-08-20 Published:2021-08-30

摘要: 滇中富民县宝石洞岩溶地下河洞穴景观系统规模适中,洞内岩溶景观千姿百态,洞中有宝(玛瑙),洞外有优美的生态环境和多元民族宗教文化以及潜在的温泉资源,加上优越的交通区位,旅游要素集群度较高,具较高开发价值。文章根据宝石洞地区区域地质背景,分析了该地区区域地史演化特征,根据本次对宝石洞的实地探测成果,总结了宝石洞旅游地质特征,再结合前人对成景机制的探讨,从岩性、构造、水文地质、古地理和成景时代五个方面探讨了宝石洞景区的成景机制,指出多期次断层(破碎带)共同控制了宝石洞景观空间格局,岩溶作用始于燕山晚期,喜山期是宝石洞岩溶地下河洞穴系统的主要成景期,并对宝石洞中产出的宝石(玛瑙)成因作了初步的推断解释。

关键词: 岩溶地下河洞穴系统, 旅游地质特征, 成景机制, 宝石洞, 滇中富民县

Abstract: The karst underground river cave landscape system in Gemstone Cave, Fumin County, Central Yunnan Province is moderate in scale with various karst landscapes in the cave, treasures (agates) in the cave, beautiful ecological environment, multiethnic religious culture and potential hot spring resources outside the cave and superior traffic location which makes the tourism elements cluster with high development value. According to the regional geological background of Gemstone Cave, this paper analyzes the evolution characteristics of regional geological history, summarizes the tourism geological characteristics of Gemstone Cave according to the field exploration results of Gemstone Cave, discusses the landscape mechanism of Gemstone Cave from five aspects: lithology, structure, hydrogeology, paleogeography and landscape age, points out that multiple faults (fracture zones) jointly control the spatial pattern of Gemstone Cave landscape. Karst started in the late Yanshan period and the Himalayan period was the main landscape period of the karst underground river cave system in Gemstone Cave. The origin of the gem (agate) produced in Gemstone Cave was preliminarily inferred and explained.

Key words: Karst underground river cave system, tourism geological characteristics, landscape mechanism, Gemstone Cave;
Fumin County,
Central Yunnan

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