摘要
藏南喜马拉雅北坡二叠系基性火山岩位于聂拉木县色龙东山。岩石地球化学特征表明,无论是基龙组火山岩还是色龙群火山岩,都具有大陆拉伸-大陆裂谷环境火山岩系的主、微量元素地球化学特征。据此,判断两套基性火山岩的性质和喷发构造环境相同。该区二叠纪大陆拉伸-裂谷火山活动标志着冈瓦纳超级古大陆开始裂离、解体。
Permian basic volcanic rocks are located in the Eastern Mountains of Selong,Nyalam County,on the northern slope of the Himalayas,southern Tibet.Volcanic rocks of both the Jilong Formation and the Selong Group show major element ,trace element and REE geochemical characteristics of the volcanic series occurring in the continental extensional-rift environments.Therefore,the natures and eruptive tec-tonic environments of the two suites of volcanic rocks are the same.The Permian continental extensional-rift volcanism in the area marked the beginning of break-up of the supercontinent Gondwana.
出处
《地质通报》
CAS
CSCD
北大核心
2002年第11期717-722,共6页
Geological Bulletin of China
基金
青藏高原1:25万聂拉木县幅区域地质调查项目(19991300009031)成果。
