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陕北甘泉丹霞峡谷群地质遗迹景观特征与保护利用
引用本文:丁 华1,2,段丰浩3,陈姗姗1,2,廖文强1,2,李永军4. 陕北甘泉丹霞峡谷群地质遗迹景观特征与保护利用[J]. 延边大学学报(自然科学版), 2023, 0(2): 362-372. DOI: 10.19814/j.jese.2022.05003
作者姓名:丁 华1  2  段丰浩3  陈姗姗1  2  廖文强1  2  李永军4
作者单位:(1. 长安大学 建筑学院,陕西 西安 710061; 2. 陕西省黄河科学研究院,陕西 西安 710054; 3. 长安大学 地质工程与测绘学院,陕西 西安 710054; 4. 长安大学 地球科学与资源学院,陕西 西安 710054)
摘    要:甘泉丹霞峡谷群位于陕北丹霞地质遗迹景观带的中部,地处鄂尔多斯盆地伊陕斜坡,为典型的狭缝式丹霞景观。通过野外调查、实测和研究发现:甘泉丹霞峡谷群地质遗迹景观的造景地层为下白垩统洛河组风成相紫红色碎屑沉积岩,岩石呈厚—巨厚层状; 垂向节理较为密集,NE—NEE向、近SN向和NW向节理控制了峡谷群的发育。景观类型以负地形的波浪谷(波浪状凹槽与凸起间或分布)为主,辅以丹霞崖壁、一线天、壶穴、象形石等; 景观类别与众不同,为具有国际对比研究价值的黄土覆盖型,主要沿洛河支流展布; 景观美学上呈现“窄狭、多弯、纵高、陡峻”+“巨厚、均一、韵律、多彩”特征; 景观价值上具有科学研究、科考探险、旅游休闲、科普教育等复合多元的多种功能。由于甘泉丹霞峡谷群地处生态环境脆弱区和经济欠发达区,未来应加大地质遗迹科研力度,划定地质遗迹保护区,明确地质遗迹保护措施,推进地质遗迹科普教育,开展地质文化村建设,以达到持续保护利用的目的。

关 键 词:丹霞地貌  地质遗迹  景观特征  黄土覆盖型  狭缝式  波浪谷  保护利用  陕西

Characteristics,Protection and Utilization of the Canyons of Danxia Landscape Geoheritages in Ganquan Area of the Northern Shaanxi,China
DING Hua1,' target="_blank" rel="external">2,DUAN Feng-hao3,CHEN Shan-shan1,' target="_blank" rel="external">2,LIAO Wen-qiang1,' target="_blank" rel="external">2,LI Yong-jun4. Characteristics,Protection and Utilization of the Canyons of Danxia Landscape Geoheritages in Ganquan Area of the Northern Shaanxi,China[J]. Journal of Yanbian University (Natural Science), 2023, 0(2): 362-372. DOI: 10.19814/j.jese.2022.05003
Authors:DING Hua1,' target="  _blank"   rel="  external"  >2,DUAN Feng-hao3,CHEN Shan-shan1,' target="  _blank"   rel="  external"  >2,LIAO Wen-qiang1,' target="  _blank"   rel="  external"  >2,LI Yong-jun4
Affiliation:(1. School of Architecture, Chang'an University, Xi'an 710061, Shaanxi, China; 2. Shaanxi Academy of Yellow River Sciences, Xi'an 710054, Shaanxi, China; 3. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 4. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China)
Abstract:The canyons of Danxia landscape in Ganquan area of the northern Shaanxi, are located in the middle part of the Danxia landscape belt, which belongs to the Yishan slope of Ordos Basin in the view of the geological structure unit. The canyons are the typical slit-typed Danxia landscapes. Through field investigations and surveys, it is confirmed that the landscape formations of canyons are red clastic sedimentary rocks of eolian facies in Lower Cretaceous Luohe Formation and the rock is thick. There are few faults, but vertical joints of NE—NEE, nearly SN and NW directions are exceptionally well developed, which control the development of canyons. The landscape type is dominated by wave valley of negative topography, and supplemented by the Danxia cliff, thin strip of sky, pothole, and pictographic stones. For the landscape category, the canyons of Danxia landscape are the kind of loess-cover type with international comparative research value. The landscape aesthetics characteristics present “narrow, multi curved, vertically high and steep”, as well as “thick, homogeneous, rhythmic and colorful”. For the landscape value, the canyons of Danxia landscape have compound and multivariate functions such as scientific research, scientific exploration, tourism and leisure, popular science education, etc. Since canyons are located in the fragile ecological environment area and underdeveloped economy area, it is necessary for Danxia geoheritages to strengthen scientific research, clarify the protection measures, promote popular science education, and carry out the construction of geologic cultural villages, in order to achieve the goal of sustainable protection and utilization.
Keywords:Danxia landform   geoheritage   landscape characteristic   loess-cover type   slit-typed   wave valley   protection and utilization   Shaanxi
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