金鞭溪地貌及其形成机制和演变过程——对张家界地貌的再认识  

The Mechanism of Forming the Physiognomy in Jinbianqi and its Process of Evolvement——Recognition of Physiognomy of Zhangjiajie

作　　者：周学军[1] 夏卫生[1] 谭长银[1] 

机构地区：[1]湖南师范大学资源与环境科学学院地理系,中国长沙410081

出　　处：《湖南师范大学自然科学学报》2004年第3期95-96,F003,共3页Journal of Natural Science of Hunan Normal University

基　　金：国家自然科学基金(40171062);中科院知识创新研究资助项目(KZCX3 SW 422)

摘　　要：张家界核心景区,以鞭状塔式石柱岩峰为特征的地貌群体,由富含节理的厚层石英砂岩构成.其正处于一个向斜扬起端,在新构造运动推动下,受扇形辐聚式水系侵蚀和重力等作用塑造而成.按其特殊的形成机理、形态特征和分布规律,提出了"金鞭溪地貌"这一新的复式命名.The physiognomy characteristic of the core scope in Zhangjiajie is mainly made of stelae rock apex pattern as scourging pagoda, structured with thick layer quartz sandstone, which is molded by the erosion of sector spoke assembling style and gravity promoted by the newly constituting movement, locating at the upwards extremity. According to the special forming mechanism, form characteristic and distribution disciplinarian, a new duplicate naming of 'physiognomy of Jinbianqi' is put forward.

关 键 词：地貌 新构造运动 向斜 石柱 形成机制 水系 重力 张家界 景区 再认识 

分 类 号：F592[经济管理—旅游管理]