桂林穿山岩溶地质遗迹特征、成因与保护对策
Characteristics, Genesis and Protection Strategies of Karst Geological Heritages in Chuanshan, Guilin
摘要: 依托既有地质背景资料，运用无人机倾斜摄影建模技术、遥感解译技术及岩溶微地貌调查相结合的方法，查明桂林穿山的构造特征，系统梳理穿山溶洞地质遗迹类型，阐述典型化学沉积遗迹的岩溶动力学演化机制。研究表明：(1) 穿山宏观上的形貌发育受NW向主控断裂和EW向横张断裂共同控制；(2) 悬挂石柱遗迹景观是古气候突变和构造抬升共同作用的产物；(3) 石盾的发育形态及鹅管–石钟乳的演化受裂隙产状、静水压力和渗流水流态的控制。本文提出建立地质遗迹数字化模型、划定绝对保护区及优化地质理论成果转化等措施保障地质遗迹资源的可持续利用。
Abstract: Based on existing geological background data, utilizing a combined method of Unmanned Aerial Vehicle (UAV) oblique photogrammetry modeling, remote sensing interpretation, and karst micro-geomorphological surveys, this study ascertains the structural characteristics of Chuanshan in Guilin, systematically categorizes the types of geological heritages in the Chuanshan caves, and elucidates the karst dynamic evolution mechanisms of typical chemical sedimentary heritages. The research indicates that: (1) the macroscopic morphological development of Chuanshan is jointly controlled by NW-trending major faults and EW-trending transverse extensional faults; (2) the suspended stone pillar heritage landscape is the product of the combined effects of abrupt paleoclimatic changes and tectonic uplift; (3) the developmental morphology of cave shields and the evolution of soda straw-stalactites are controlled by fracture attitudes, hydrostatic pressure, and seepage flow regimes. To ensure the sustainable utilization of geological heritage resources, this paper proposes measures such as establishing digital models of geological heritages, delineating absolute protection zones, and optimizing the transformation of geological theoretical achievements.
文章引用：王法骏. 桂林穿山岩溶地质遗迹特征、成因与保护对策[J]. 地球科学前沿, 2026, 16(7): 1005-1017. https://doi.org/10.12677/ag.2026.167090

参考文献

[1] 袁道先, 章程. 岩溶动力学的理论探索与实践[J]. 地球学报, 2008(3): 355-365.
[2] 陈志强, 张远海, 邓亚东. 凤山岩溶国家地质公园溶洞资源特征及保护价值评价[J]. 资源环境与工程, 2025, 39(6): 771-779.
[3] 贾志远, 弓小平, 王吉润, 等. 新疆特克斯县科桑溶洞地质遗迹特征、成因及评价[J]. 城市地质, 2025, 20(1): 60-69.
[4] 潘天望, 史文强, 李成展, 等. 云南麻栗坡老山地区岩溶地貌地质遗迹特征及成因分析[J]. 中国岩溶, 2024, 43(6): 1430-1444.
[5] 江志, 汪梅生. 安徽石台溶洞群国家地质公园溶洞群地质成因简析[J]. 西部资源, 2022(4): 182-184.
[6] 任娟刚, 洪增林, 唐力, 等. 陕西镇巴三元天坑群岩溶地质遗迹特征及成因[J]. 四川地质学报, 2021, 41(3): 523-528.
[7] 洪增林, 任娟刚, 张远海. 陕西汉中天坑群岩溶地质遗迹形成探微[J]. 陕西理工大学学报(自然科学版), 2020, 36(3): 81-87.
[8] 陈武, 肖加飞, 谯文浪, 等. 贵州施秉喀斯特世界自然遗产地地质遗迹类型和特征[J]. 贵州科学, 2020, 38(1): 62-70.
[9] Bazebizonza Tchiguina, N.C., Samba, P.R.R., Nkodia, H.M.D., Boudzoumou, F., Arfaoui, I., François, C., et al. (2026) Inventory of Karstic Cavities of the Schisto-Calcaire Group, Republic of the Congo: Applying a Geoheritage Promotion Approach in the Madingou Region. International Journal of Geoheritage and Parks, 14, 43-59. [Google Scholar] [CrossRef] 
[10] Singtuen, V., Nulay, P., Kaweera, A., Charoentitirat, T. and Phajuy, B. (2024) Geoheritage Characterisation of Thap Lao Karst Spring in Chaiyaphum Geopark, Northeastern Thailand for Sustainable Geotourism Development. Geoheritage, 16, Article No. 113. [Google Scholar] [CrossRef] 
[11] 范可, 冯佐海, 王翔, 等. 桂林市岩质崩塌发育特征与影响因素[J]. 自然灾害学报, 2019, 28(2): 169-182.
[12] 冯佐海, 李晓峰, 刘辉利, 等. 桂林市断裂构造对岩溶塌陷的控制作用[J]. 桂林工学院学报, 2000, 20(4): 344-349.
[13] 颜李冰清. 桂林市岩溶塌陷发育特征及发展趋势分析[D]: [硕士学位论文]. 桂林: 桂林理工大学, 2022.
[14] 江思义, 吴福, 刘庆超, 等. 广西桂林市规划中心城区岩溶塌陷时空分布规律及成因分析[J]. 中国地质灾害与防治学报, 2020, 31(3): 65-72.
[15] 吴枝坦. 桂林市地下岩溶发育规律性的初步探讨[J]. 广西地质, 1986(1): 76-84.
[16] 袁道先, 等. 现代岩溶学[M]. 北京: 科学出版社, 2016: 34.