CHARACTERISTICS AND REGIONALIZATION OF THE GEOLOGICAL RELIC RESOURCES IN SHUNPING COUNTY, HEBEI PROVINCE
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摘要:
河北省顺平县是太行山区与华北平原的典型过渡区域.该区地质遗迹资源丰富,类型多样,在太行山北段具有较好代表性.经县域范围内的详细调查,查明顺平县地质遗迹资源共3大类、10类、16亚类,合计地质遗迹点33处.对各类地质遗迹的分布特征做了描述,并进行了相关区划研究,划分出3个地质遗迹分布区和5个地质遗迹集中区,结合区域特征、遗迹数量、其他旅游资源和保护开发前景等因素,为县域范围内地质遗迹资源保护与开发提供基础数据.该成果一方面能够有效支撑和服务顺平县脱贫攻坚成果,促进当地旅游发展和规划,同时也能为进一步推进县市范围的大比例尺地质遗迹详细调查与研究提供一定的参考和示范.
Abstract:Shunping County of Hebei Province is geographically a typical transition between Taihang mountainous area and North China plain, with rich and diverse geological relic resources, which is representative of the northern Taihang Mountains. According to the detailed survey in the county, the geological relics can be classified into 3 categories, including 10 groups and 16 subgroups, with a total of 33 geological relic sites. This paper analyzes the distribution features of each geological relic and related regionalization, and delineates 3 distribution areas and 5 concentration areas of geological relics. Combined with regional characteristics, relic numbers, other tourism resources and protection-development prospects, the paper provides basic data for protection and development of geological relic resources in the county. The survey result can effectively support and serve the poverty alleviation achievement and promote the local tourism development and planning. Besides, it can also provide some reference and example for detailed survey and study of large scale geological relics in counties and cities.
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Key words:
- geological relic /
- regionalization /
- geological survey plus /
- Shunping County /
- Hebei Province
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表 1 河北省顺平县地质遗迹资源分类表
Table 1. Classification of geological relic resources in Shunping County, Hebei Province
大类 类 亚类 数量/处 基础地质 地层剖面 典型剖面 1 岩石剖面 侵入岩剖面 1 构造剖面 不整合面 2 褶皱与变形 2 断裂 2 重要化石产地 古植物化石产地 1 重要岩矿石产地 矿业遗迹 3 地貌景观 岩土体地貌 碳酸盐岩地貌(岩溶地貌) 9 水体地貌 河流(景观带) 2 湖泊、潭 1 瀑布 1 泉 3 冰川地貌 古冰川遗迹 1 构造地貌 峡谷 2 地质灾害 地质灾害遗迹 滑坡 1 地面塌陷(地裂缝) 1 表 2 顺平县地质遗迹区划特征表
Table 2. Characteristics of geological relic regionalization in Shunping County
分布区 集中区 集中区特征 地质遗迹主要类型 数量 其他特色旅游资源 重要性 开发前景 顺平县冲洪积平原分布区(I) 地貌上为冲洪积平原区, 地表第四系覆盖较为严重, 无明显露头, 可见的地质遗迹资源出露较少 地质灾害遗迹, 其他遗迹资源覆盖较大, 无明显出露 1 腰山王氏庄园和伍侯塔等历史文化遗迹 次要 不具有开发价值 顺平县低山丘陵地质遗迹分布区(II) 清醒村-龙堂村地质遗迹集中区(II1) 地貌上为低山丘陵, 出露岩性主要为古生代砂岩、灰岩, 受区域构造影响, 遗迹点多为构造成因, 遗迹点分散 以构造剖面为主, 此外还有典型剖面和岩土体地貌 5 大悲水库、万青山、秀兰山庄和大佛光寺等 次要 不具有开发价值 伊祁山-火焰山地质遗迹集中区(II2) 地貌上为低山丘陵, 出露岩性主要为中元古代灰岩、白云岩, 遗迹点多分布在宽缓的孤山周边, 遗迹点较分散 岩土体地貌、水体地貌、重要岩矿石产地 8 伊祁山、马耳山、火焰山、万顷桃园农庄民俗园等 次要 可适当开发 杨家台地质遗迹集中区(II3) 地貌上为低山丘陵, 出露岩性主要为中元古代灰岩、白云岩, 遗迹点沿界河呈带状分布, 遗迹点分布较集中 构造剖面、矿业遗迹、岩土体地貌及水体地貌 5 享水溪、红色抗战遗迹、界河景观带等 重要 可适当开发 顺平县中山地质遗迹分布区(III) 白银坨地质遗迹集中区(III1) 地貌上为中山, 岩性主要为中元古代白云岩, 遗迹点分布集中, 主要在白银坨-寨沟景区周边, 具有较大的开发潜力 岩土体地貌为主, 见岩石剖面、矿业遗迹、重要化石产地、水体地貌、冰川地貌、构造地貌 9 白银坨森林公园和龙潭湖 重要 重点开发 杏唐沟-三妙峰地质遗迹集中区(III2) 地貌上为中山-河谷, 岩性主要为中元古代白云岩, 主要分布唐河两岸, 尤以杏唐沟-三妙峰景区为典型, 遗迹点分布较集中 岩土体地貌和水体地貌 4 杏唐沟景区、华北第一洞漂、三妙峰景区 重要 重点开发 -
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