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越南岩溶地质概况

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越南岩溶发育面积大,岩溶地质有关研究比较广泛,为了更全面地掌握越南岩溶地质的研究成果,本文综合分析前人研究成果,结合遥感资料、地质图、洞穴图集等有关资料,编制越南岩溶地质分布图,结合地质构造、岩性组合、水文气候、生物活动等特征分析岩溶作用的背景条件,总结越南岩溶地质、地貌特征和岩溶分布规律,为"全球岩溶地质"数据库提供基础支持.越南岩溶分布面积60 000 km2,占国土面积的20%,主要分布在越南的北部和中部,南部有零星分布,发育峰丛、峰林、岩溶盆地、洞穴等岩溶景观.多期构造运动、厚层石炭系—二叠系、三叠系纯石灰岩、温润多雨的热带季风气候、活跃的生物活动均有利于岩溶作用的发生.越南岩溶属于典型的热带岩溶,与中国南部岩溶具相似的起源.
Overview on karst geology of Vietnam
Karst is widely distributed in Vietnam,covering almost 60,000 km2,approximately 20%of the total area of Vietnam.Most karst rocks crop out in North and Central Vietnam.Karst developed with peak-clusters,peak-forests,caves,etc.is sparsely distributed in the south of Vietnam.Based on previous research,the geological map of karst distribution in Vietnam was drawn up,combined with remote sensing image,geological map,and cave atlas.In terms of geological structure,lithology combination,hydroclimate in Vietnam,conditions of karstification in this country were analyzed.From the perspective of regional geology,the characteristics of karst geology and geomorphology,karst distribution and the present situation of karst resources in Vietnam were investigated.Karst in Vietnam is distributed in the tropical karst belt,with similar origins of karst in South China.The distribution law of karst in Vietnam is mainly controlled by stratigraphic lithology and tectonic movement.Karst is developed in all the pre-Cambrian and Holocene strata and the pure limestone strata of Carboniferous,Permian and Triassic with a thickness of 1,000-2,000 m are the main beds of karst development.The warm and rainy climate and rich biological diversity accelerate karstification.There are four major karst zones in Vietnam,including peak-clusters and peak-forests in the northeast,peak-forests in Ha Long Bay and karst mountain along Truong Son Ra karst in the northwest.The karst area in northeast is an extension of the karst from South China,with the development of alpine karst landforms,peak-forests,peak-clusters,large drainage gullies and sinkholes.Sinkholes are extremely developed,with an average 1.4 sinkholes per square kilometer.The karst landforms vary from plateaus to depressions and hills and finally to plains from northwest to southeast,showing a complete evolution of tropical karst geomorphology.There are karst landforms such as large and deep poljes,deep gullies and caves.The vertical distance of Conh Nuoc cave,the deepest cave,is 600 m.The peak-forest along Ha Long Bay is an extension of the peak-forest of South China.In the central part,karst is distributed along the Truong Son Ra.Phong Nha Cave currently known as the longest cave in Vietnam is located in the famous karst area of Phong Nha-Ke Bang.The Phong Nha cave system is composed of 20 caves,more than 60 km in length,where is located the longest river cave and the cave with the largest passage in the world.Vietnam is rich in karst water,karst mineral and karst landscape resources.At present,karst water has become the main water source for industry,agriculture and life in Vietnam,but water supply is in serious shortage,especially in the dry season.Vietnam is at an advanced level in the exploitation of karst mineral resources and is currently the eighth largest cement producer in the world.Remarkable achievements have been made in balancing regional economic development and ecological protection,and a series of world geological heritage reserves and national ecological reserves have been established in karst areas.

Vietnamkarst geologykarst landscapekarst resources

韦延兰、李文莉、黄晨晖、周立新、杨象鹏

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中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心,广西桂林 541004

广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406

越南 岩溶地质 岩溶景观 岩溶资源

中国地质科学院岩溶地质研究所基本科研业务费

2002372017001

2024

中国岩溶
中国地质科学院岩溶地质研究所

中国岩溶

CSTPCD北大核心
影响因子:0.908
ISSN:1001-4810
年,卷(期):2024.43(2)