新疆昭苏夏塔冰川地貌特征及成因分析  

Glacial Landforms and Their Genesis in Xiata,Zhaosu,Xinjiang

作　　者：杨林[1] 邓强 沈洪江[1] YANG Lin;DENG Qiang;SHEN Hong-jiang(Regional Geological Surveying Team,BGEEMRSP,Chengdu 610213;China Geological Engineering Group Co.Ltd.,Ürümqi 850063)

机构地区：[1]四川省地质矿产勘查开发局区域地质调查队,成都610213 [2]中国地质工程集团有限公司,乌鲁木齐860063

出　　处：《四川地质学报》2021年第S02期151-155,共5页Acta Geologica Sichuan

基　　金：新疆维吾尔自治区国土资源厅昭苏县夏塔地质遗迹调查与评价项目(项目编号:XJYJDC2017-04)资助。

摘　　要：夏塔位于新疆哈尔克山北麓和昭苏盆地之间,处于西天山造山带的核心部位,该地区在漫长的地质历史时期中,在各种地质营力的综合作用下,形成了以冰川地貌为主体的地质遗迹景观资源。在野外系统调查的基础上,总结了研究区冰川地貌具有空间分带性特征,冰川地貌以现代冰川为核心、四周发育着众多以典型冰蚀地貌为主要特征的古冰川地貌,辅以冰川堆积地貌和冰水沉积地貌,观赏价值较高。通过冰川地貌成因分析,进一步提升冰川地貌的科学内涵,为景区开发建设提供科学依据。Xiata lies between thenorth foot of the Halik Mountain and the Zhaosu basin in the core of the west Tianshan orogenic zone.Landscape resources of geoheritage with glacial landforms as main body were formed here due to the combined action of various geological agents during long geological history.The glacial landforms are characterized by zonation with contemporary glacial landforms in the core and a great amount of former glacial landforms characterized by typical glaciated landform,and glacial deposition landform and glaciofluvial deposit landformall around.The glacial landforms in Xiataare of high ornamental value.

关 键 词：夏塔 冰川地貌 现代冰川 古冰川 成因分析 

分 类 号：P66[天文地球—地质学]