Volcanic geology of Admiralty Bay,King George Island,Antarctica

被引:0
|
作者
邢光福
王德滋
金庆民
沈渭洲
陶奎元
机构
[1] China
[2] Nanjing Institute of Geology and Mineral Resources
[3] Nanjing Institute of Geology and Mineral Resources Nanjing 210016
关键词
caldera; temporal-spatial evolution; Tertiary volcanism; Admiralty Bay; King George Island;
D O I
暂无
中图分类号
P317 [火山学];
学科分类号
070801 ;
摘要
At Admiralty Bay of central King George Island, Keller Peninsula, Ull-man Spur and Point Hennequin are main Tertiary volcanic terranes. Field investigation and isotopic datings indicate that, there occurred three periods of eruptions ( three volcanic cycles) and accompanying N-toward migration of the volcanic center on Keller Peninsula. After the second period of eruptions, the crater collapsed and a cal-dera was formed, then later eruptions were limited at the northern end of the peninsula and finally migrated to Ullman Spur. Thus Keller Peninsula is a revived caldera, and its volcanism migrated toward E with time. Point Hennequin volcanism happened more or less simultaneously with the above two areas, but has no clear relation in chemical evolution with them, frequently it belongs to another independent volcanic center.
引用
收藏
页码:89 / 102
页数:14
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