摘要
对柯林斯冰帽小冰穹冰芯中物质成分的研究,发现冰芯中有九层火山灰沉积。它们由玻屑(橙玄玻璃)、岩屑(黑色)和晶屑(长石、辉石、橄榄石和微量的钛铁氧化物)组成。长石为钠钙系列的中长石到拉长石。橄榄石为镁质的贵橄榄石。主要元素和微量元素分析结果表明,该类火山灰为玄武质成分,其SiO2含量在50wt%左右,Na2O大于K2O,并具有轻稀土元素轻微的富集、重稀土元素亏损、Eu正异常的特征。这些火山灰的存在,证实了近百年来南极地区的企鹅岛和欺骗岛的火山喷发活动。
According to our study,there are nine layers ot volcanic ash deposited in ice core of small dome from Collins cap,King Creorge Island of Antarctica.These volcanic ashes consist of black color volcanic detritus,yellow volcanic glass and crystal mineral that are plagioclases,clinopyroxenes,olivine and a few of amphiboles, Ti-Fe oxides. The plagioclases belong to albite-anorthic series(An=33~55). Olivine is chrysolite type (Fo= 70~74). Major elements and trace elements analyses of volcanic ashes suggest that they are tholeiite with richer soda and lower potassium features. The REE distribution patterns of these ashes show light REE enriched type. Characteristics of expending mineral chemistry and geochemistry indicate that the ice core has a record of volcanic activity event nearly 100 years in Deception island and Penguin island of southwest Antarctica.
出处
《岩石学报》
SCIE
CAS
CSCD
北大核心
1996年第3期434-445,共12页
Acta Petrologica Sinica
基金
国家南极考察委员会资助
中国科学院资助
关键词
冰帽
冰芯
火山物质
成分
南极
Composition
Volcanic Ash
Ice core
Antarctica