极地研究 ›› 1991, Vol. 3 ›› Issue (3): 25-38.

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南极乔治王岛菲尔德斯半岛冰缘地貌过程分析

朱诚;崔之久;熊黑钢   

  • 出版日期:1991-09-30 发布日期:1991-09-30

AN ANALYSIS OF PERIGLACIO-GEOMORPHIC PROCES-SES ON FILDES PENINSULA, KING GEORGE ISLAND, ANTARCTICA

  • Online:1991-09-30 Published:1991-09-30

摘要:

根据定位重复测量、坑探、物探、人工灌水、地温资料和样品室内分析,作者讨论了菲尔德斯半岛石冰川、倒石堆、分选环、石花、流动性条纹土等冰缘地貌变化过程和沉积结构特征,论证了含盐量对电阻率和冰缘地貌物质迁移的影响,最后指出了本区冰缘研究的问题。

关键词: 冰缘地貌过程;含盐量;石花;条纹土;沉积结构

Abstract:

This paper deals with the periglacio-geomorphic processes on the Fildes Peninsula, King George Island, Antarctica. Based on the works of fixed repeated surveying, pitting, geoelectrical prospecting, artificial watering, geothermal measurement and the sample analysing, the authors discussed perigiacio-geomorphic processes and sediment structural feature of rock glacier, talus, sorted circles, debris flower, striated soil, and proved the influence of salty sediments to electric resistivity and substantial migration. Rock glacier and striated soil are active in summer season, stone circles can be divided into two types: beach gravel-type with convex-shaped table and debris type with bowl- shaped frost table. Resistivity of salty sediments can lowly reach to 2.9×10' -7×102Ω m. Those phenomena are concordant with the typical characteristics of Sub-Antarctic Island Type periglacial geomorphology. Finally, the problems of periglacial research work in this area are also pointed out by the authors.