摘要
湖南南部西山火山 侵入杂岩中 3个代表性岩石单元 (花岗岩、碎斑熔岩和流纹岩 )的产状、岩石化学、微量元素和同位素地球化学特征显示 ,它们同空间、同物质来源。全岩Rb Sr定年结果表明 :花岗岩、碎斑熔岩和流纹岩的形成时代分别为15 6± 6Ma、15 9± 2Ma和 15 4± 11Ma ,87Sr/86Sr初始值分别为 0 .71779、0 .71738和 0 .71774 ,其中碎斑熔岩的锆石SHRIMP定年结果为 15 6± 2Ma ,它们在误差范围内基本相同 ,为中侏罗世晚期同一构造岩浆事件中陆壳活化的产物。
The occurrences, geochemistry and trace element and isotopic characteristics of three representative rock units, namely granite, clastoporphyritic lava and rhyolite, in Xishan granitic volcanic-intrusive complex of southern Hunan, indicate that they have identical space and material resources. The whole rock Rb-Sr dating shows that the ages of these three units are 156±6 Ma,159±2 Ma and 154±11 Ma, respectively, and the zircon SHRIMP age of the clastoporphyritic lava is 156±2 Ma. These age data show that the Xishan complex was formed almost at the same time, and might have been the late stage product of the Middle Jurassic magmatism.
出处
《地球学报》
EI
CAS
CSCD
北大核心
2004年第3期303-308,共6页
Acta Geoscientica Sinica
基金
宜昌地质矿产研究所科技发展基金 (编号 :K2 0 0 3 0 2 )
中国地质调查局基础地质综合研究项目 (编号 :2 0 0 113 90 0 0 18)资助