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大兴安岭北段塔木兰沟组玄武岩地球化学及构造背景
GEOCHEMICAL CHARACTERISTICS AND TECTONIC BACKGROUND OF BASALT FROM TAMULANGOU FORMATION IN NORTHERN DAXINGANLING
【摘要】 通过对大兴安岭北段塔木兰沟组玄武岩岩石学、地球化学及其形成的大地构造环境的综合研究发现,塔木兰沟组玄武岩具有拉斑玄武岩和碱性玄武岩的双重特征,Na2O-2<K2O;Eu无异常,La/Yb=35.7(平均);富集Ba、Sr、K,亏损Nb.岩浆的形成可能与裂谷作用有关.在这一构造-热事件中,推测该裂谷在上黑龙江地区陆壳减薄最大,呼中地区岩石圈减薄最大,根河地区陆壳、岩石圈减薄均较小.
【Abstract】 Study on the petrology,geochemistry and tectonic setting of the basalt from Tamulangou formation indicates that the basic volcanic rocks are geochemically similar to both tholeiitic basalt and alkali basalt,with Na2O-2< K2O,no negative Eu anomaly,La/Yb=35.7,rich Ba,Sr and K,and deficient Nb.The magma is probably generated by rifting.In such a thermal-tectonic event,it is speculated that the crust in Shangheilongjiang area and the lithosphere in Huzhong area were thinned greatly;while the lithosphere and the crust in Genhe area were slightly thinned.
【Key words】 basalt; rifting; Tamulangou formation; Northen Daxinganling;
- 【文献出处】 地质与资源 ,Journal of Precious Metallic Geology , 编辑部邮箱 ,2005年02期
- 【分类号】P588.145;P59
- 【被引频次】57
- 【下载频次】586