| 毕节鸡鸣三省?贵州地质公园地质遗迹特征及价值研究 |
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| 引用本文： | 罗书文,杨桃,邓亚东,覃星铭.毕节鸡鸣三省?贵州地质公园地质遗迹特征及价值研究[J].中国岩溶,2019,38(6):946-956. |
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| 作者姓名： | 罗书文 杨桃 邓亚东 覃星铭 |
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| 作者单位： | 1.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，广西 桂林 541004 |
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| 基金项目： | 国家自然科学青年基金（41502257）；中国地质科学院院长基金（YYWF201638）；中国地质大调查（DD20160285、DD20179313、DD20160061）；毕节鸡鸣三省?贵州地质公园申报（300021000001609005） |
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| 摘 要： | 为了探讨毕节鸡鸣三省?贵州地质公园地质遗迹发育特征及旅游开发价值，本文在实地调查基础上，系统分析了公园内地质遗迹的类型与发育特征，根据地质遗迹景观的评价体系和方法对地质遗迹景观进行定性和定量研究。结果表明:（1）公园地处云贵高原向四川盆地过渡的斜坡地带，是斜坡带岩溶地貌的典型代表；（2）从分水岭到赤水河谷，岩溶地貌表现为由峰丛洼地→溶丘洼地→岩溶峡谷的系列变化，具有显著的地带分异性，展现了岩溶地貌在水文单元系统中的发育规律；（3）资源景观类型互补性强，具有极高的科研、观赏和旅游开发价值；（4）园区地质遗迹类型共分为6大类10类10亚类，以岩溶峡谷、洞穴、天生桥、天坑、峰丛、溶丘、石林、象形山等岩溶地貌为主，以水体景观、地质剖面、古生物、环境地质遗迹和地质构造遗迹为辅。园区内有国家级地质遗迹3处，省级地质遗迹11处。
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| 关 键 词： | 毕节鸡鸣三省 地质公园 地质遗迹特征 价值研究 岩溶地貌 |
Characteristics and value of geological relics in the Bijie Jiming Sansheng?Guizhou geopark |
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| LUO Shuwen,YANG Tao,DENG Yadong and QIN Xingming.Characteristics and value of geological relics in the Bijie Jiming Sansheng?Guizhou geopark[J].Carsologica Sinica,2019,38(6):946-956. |
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| Authors: | LUO Shuwen YANG Tao DENG Yadong and QIN Xingming |
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| Institution: | 1.Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR&GZAR，Guilin，Guangxi 541004，China2.Number Twelve Middel School of Guiyang , Guiyang, Guizhou 550002,China |
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| Abstract: | This paper explores the characteristics and value of geological relics in the Bijie Jiming Sansheng ? Guizhou geopark. Based on field investigations, we study the types and development characteristics of the geological relics in the park, and make qualitative and quantitative evaluation to its landscape. Our research suggests that， (1) The Bijie Jiming Sansheng ? Guizhou geopark is a typical representative of karst in the slope of the transition from the Yunnan-Guizhou plateau to the Sichuan basin； (2) From the watershed to the Chishui River valley, the karst landform changes are expressed by peak cluster depressions e karst doom depressions kkarst canyons with significant zoning, showing the development of karst landforms in the hydrological unit system； (3) The resource landscape types are complementary and have high values for research, ornamental and tourism development；(4) The types of geological relics in the park are divided into six big categories, ten small categories and ten sub-categories, dominated by karst gorges, caves, natural bridges, Tiankeng, peak clusters, karst dooms, stone forests and pictographic mountains, with waterscapes, geological sections, paleontology, environmental geological relics and geological structure relics as complements. Our work determines 3 national-level geogoical relics and 11 provincial-level geological relics in the park, which provides a basis for rational development and protection of geological relics in the park and advancing local tourism industry. |
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