摘要
柯树北岩体为陆壳改造型（S型）花岗岩，具有结构和成分演化序列。运用岩石结构序列法，将其划分为6个单元，归并为1个超单元。按侵入体空间展布形式、岩体地质学、岩石学、构造地球化学等资料，提出了岩浆侵位是受区域拉张应力控制的认识。
： The Keshubei intrusion is composed of a continental crust transformation type (S－type) granite and displays a textural and compositional evolution sequence． With a rock textural sequential method, this granite is divisible into 6 units which are combined into one superunit． Based on the geometry of the intrusion, rock geology, petrology and tectono－geochemistry, the author believes that the emplacement of this granite has been controlled by regional tensile stress．
出处
《江西地质》
2001年第1期22-28,共7页
Jiangxi Geology
