华北北缘固阳二叠纪闪长岩-石英闪长岩-英云闪长岩套SHRIMP年代学  

SHRIMP dating of the Permian Guyang diorite-quartz diorite-tonalite suite in the northern margin of the North China Craton

作　　者：张维[1] 简平[1] 

机构地区：[1]中国地质科学院地质研究所,北京100037

出　　处：《中国地质》2012年第6期1593-1603,共11页Geology in China

基　　金：中国地质调查局地质调查工作项目(1212011121071)资助

摘　　要：应用岩石地球化学方法,笔者在内蒙古二叠纪索伦山蛇绿岩缝合带南100～180 km、华北克拉通北缘固阳地区,识别出了一个闪长岩-石英闪长岩-英云闪长岩套。这些花岗质岩石为钠质,与岛弧深成岩在化学成分上一致。SHRIMP年代学研究表明:2件闪长岩的SHRIMP U-Pb锆石年龄为(293±4)Ma和(266±4)Ma;1件石英闪长岩的锆石年龄为(272±7)Ma;1件英云闪长岩的锆石年龄为(277±3)Ma。这些二叠纪花岗质岩石因此在形成时代上没有间断,它们与索伦山SSZ(supersubduction zone)型蛇绿岩(299～290 Ma)大致同时或略晚。基于其特定的构造背景及其与索伦山蛇绿岩的时代关系,所研究的二叠纪钠质深成岩套(293～266 Ma)与大致同时代的安山质火山岩一起,构成一个大陆边缘岛弧。Using a petrogeochemical means,we recognize a diorite-quartz diorite-tonalite suit in the northern margin of the North China craton,some 100-180 km south of the Permian Solonker ophiolite-decorated suture.The granitoid rocks are all sodic,consistent in composition with a plutonic arc.SHRIMP dating of zircons from two diorites yielded weighted mean 206Pb/238U ages of 293±4 Ma and 266±4 Ma.A quartz diorite and a tonalite are dated at 272±7 Ma and 277±3 Ma respectively.These Permian granitoid rocks were thus emplaced continuously.They are nearly coeval with,or slightly younger than,the Solonker SSZ（supersubduction zone）-type ophiolite.On the basis of a specific tectonic setting and an age relationship with the Permian Solonker SSZ-type ophiolite,we interpret the sodic granitoid suit investigated,together with near-contemporaneous andesites of the area,to form a continental margin arc.

关 键 词：大陆边缘岛弧 钠质深成岩套 锆石年龄 固阳 

分 类 号：P597.3[天文地球—地球化学]