摘要
本文从杂岩体和火山杂岩产出的地质构造环境、活动时序、岩石序列、演化规律、微量元素及锶同位素等方面讨论它们的成因联系。认为是在相同构造环境下,同期、同源岩浆在演化的不同阶段先后喷出和侵入的产物。
This paper discussed the genetic relations between the zhangzhou intrusive complex and Jianweishan volcanic complexin structural environment time sequence.rock sequence,evolutionary regularity,trace elements and Sr isotope.It is be-lieved that they are effusive and intruded and differentiation products of a co-stage and comagmatic evolution in differntstage of the same strutural environment.
出处
《福建地质》
1989年第3期217-224,240,共9页
Geology of Fujian
