九资河—天堂寨地区燕山晚期花岗岩与大别造山带核部隆升

大面积分布在大别造山带核部九资河－天堂寨地区、构成著名的天堂寨花岗质杂岩体主体的燕山晚期花岗岩，包括九资河片麻状花岗岩、吴家山花岗闪长岩、天堂寨斑状花岗岩、薄力峰细粒花岗岩和笔架山浅色花岗岩等和个岩石类型（单元）。其围岩为遭受角闪岩相区域变质和混合岩化的新太古代大别杂岩。根据其与研究区主体构造－巨型ＮＥ向右行走测韧性剪切带的关系，这些花岗岩可分为同构造、无构造和构造后等３个构造类型。从岩石角度看，

Late Yanshanian Granites in the Jiuzihe-Tiantangzhai Area and Uplift of the Core of the Dabie Orogenic Belt

Late Yanshanian granites, which are widespread in the Jiuzihe - Tiantangzhai area tangzhai granitic complex, can be grouped into 5 rocks types (units), i. e. the Jiuzihe gneissose granite, Wujiashan granodiorite, Tiantangzhai porphyritic granite, Bodaofen