| 太行大峡谷的地质景观 |
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| 引用本文： | 吴娜,李菲,吴进甫.太行大峡谷的地质景观[J].安阳工学院学报,2006(3):11-15. |
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| 作者姓名： | 吴娜 李菲 吴进甫 |
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| 作者单位： | 安阳工学院,河南,安阳,455000;安阳工学院,河南,安阳,455000;安阳工学院,河南,安阳,455000 |
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| 摘 要： | 太行大峡谷在震旦纪、寒武纪、奥陶纪为海洋,历经陆、海变迁,三迭纪中期上升为陆地,经受了200百万年的风化剥蚀,石英砂岩的差异风化形成了大峡谷独特的地质景观,现为国家4A级旅游风景区。开发大峡谷丰富的地质内涵,可提高旅游情趣,增强对大自然的保护意识。
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| 关 键 词： | 峡谷 地质发展史 景观地质特征 地质旅游 |
| 文章编号： | 1673-2928（2006）03-0010-05 |
| 收稿时间： | 2006-03-13 |
| 修稿时间： | 2006年3月13日 |
The Geological Landscape of TaiHang Great Canyon |
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| WU Na,LI Fei,WU Jin-fu.The Geological Landscape of TaiHang Great Canyon[J].Journal of Anyang Institute of Technology,2006(3):11-15. |
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| Authors: | WU Na LI Fei WU Jin-fu |
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| Abstract: | Having been an grand ocean in the Sinian period ,Cambrian period and Ordovician period, TaiHang Great Canyon rised up to the continent in Triassic period. After suffering from weathering and denudation for two hundred millions of years, the geological landscape characterastics of the TaiHang Great Canyon came into being due to the different weathering of the quartz sandstone. TaiHang Great Canyon has become one of the touring landscape ranked as the National 4A now. It is proposed that developing the rich geological meaning of TaiHang Great Canyon can improve touring joy , and enhance the protective awareness for our nature. |
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| Keywords: | canyon the developmental history of geology characteristic of geological landscape tour of geology |
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