山东岱崮地貌研究综述

摘要:

岱崮地貌是继岩溶地貌、丹霞地貌、张家界地貌、嶂石岩地貌之后的中国第5种岩石地貌，作为一种新命名的地貌类型，岱崮地貌具有极大的美学价值和科研价值。但对其的研究和开发却相对滞后。该文介绍了岱崮地貌的研究现状、分布及其形成过程、发育阶段等，岱崮地貌的分布规律、形态特征、组成结构，其演变趋势与模式及其形成机制等，是其学术研究的核心问题。加强对岱崮地貌的研究，不仅能够改变地貌学中关于方山研究的薄弱局面，丰富大陆风化及陆地碳循环研究，而且可深化对沂蒙山区地质地貌条件、生态环境特点的认识，也可为申报国家地质公园和世界自然遗产提供科学支撑。

Abstract:

Daigu landform is the fifth modeling landform after karst landform, Danxia landform, Zhangjiajie landform and Zhangshiyan landform in China. They have greatly aesthetic values and scientific values. But there is still a lack of systematic research and development and utilization. Therefore, the key topics of academic research on Daigu landform in the future is its distribution, morphological characteristics, composition structure, evolution trend, formation mechanism, etc. The research on Daigu landform can reverse current situation of weak mesa research in geomorphology field and enrich the research on continental weathering and terrestrial carbon cycle. Furthermore, it can deepen the understanding of geological and geomorphologic conditions as well as ecological features of Yimeng Mountainous area. Relevant findings will provide scientific support for applying for national geological park and the world natural heritage.