摘要
浙江大明山花岗岩是早白垩世中国东南沿海区域大规模岩浆活动的产物之一。新生代以来的地貌演变,大明山形成了丰富多样的花岗岩地貌景观,整体表现为花岗岩的峰丛地貌。通过对大明山一带花岗岩地貌的实地调查研究,本文阐述了该区花岗岩地貌的地貌分区及典型地貌景观特征,总结了大明山一带花岗岩地貌的地貌模式,并分析其成因与演化过程。
Daming Mountain granite in Zhejiang province is one of the products of Early Cretaceous China southeast coastal area large- scale magmatic activity. Since the Cenozoic evolution of landforms, Damingshan form a rich and varied landscape of granite, he overall performance of granite peak cluster landform. Through field survey and research on the Daming Mountain granite geomorphology, this paper expounds t landform zoning of Granite Landforms and typical geomorphic landscape characteristics, summarizes the landform pattern of Daming Mountain area of granite landforms, and analyse its causes and evolution.
出处
《科技通报》
北大核心
2016年第2期66-70,共5页
Bulletin of Science and Technology
基金
国家重要地质遗迹调查项目(1212011220045)
关键词
花岗岩
地貌景观
峰丛地貌
演化
浙江大明山
granite
landscape
peak cluster landform
evolution
Mt.Daming in Zhejiang province
