%0 Journal Article
%T Unique Carboniferous-Permian tectonic-metallogenic framework of Northern Xinjiang(NW China):Constraints for the tectonics of the southern Paleoasian Domain.<br>新疆北部石炭纪-二叠纪独特的构造-成矿作用：对古亚洲洋构造域南部大地构造演化的制约
%A XIAO WenJiao
%A HAN ChunMing
%A YUAN Chao
%A CHEN HanLin
%A SUN Min
%A LIN ShouFa
%A LI ZiLong
%A MAO QiGui
%A ZHANG JiEn
%A SUN Shu
%A LI JiLiang
%A <br>肖文交
%A 韩春明
%A 袁超
%A 陈汉林
%A 孙敏
%A 林寿发
%A 厉子龙
%A 毛启贵
%A 张继恩
%A 孙枢
%A 李继亮
%J 岩石学报
%D 2006
%I 
%X The late Paleozoic tectonic-metallogenic framework of North Xinjiang of the southern Paleoasian Domain was characterized by a serious of Carboniferous-Permian events,including:(1)late Carboniferous-Permian Chinese Altay island arc and its metamorphism,granulite in the Chinese Altay,radiolarian chert and high-pressure/ultra-high-pressure metamorphism;(2)late Carboniferous-early Permian adakites,Alaskan-type mafic-ultramafic complexes,and calc-alkaline magmatism,together with porphyry copper deposits,which occurred in the North Xinjiang;and(3)late Carboniferous ophiolite and island arc volcanic rocks located in the Tian Shan.Combined with the facts that there was no typical foreland basin,no typical collisional-type granitoid,and there were large amount of strike-slip faulting,it is suggested that in the Carboniferous-early Permian North Xinjiang was characterized by the coexistence of compression-extension-strike-slip structures with active magmatism and metallogeny.These phenomena all indicate that there were active margins during the late Carboniferous-early Permian,leading to the notion that the complicated aeeretionary orogeny along the southern Paleoasian Domain may have lasted to the latest Carboniferous-Permian.
%K North Xinjiang
%K Carboniferous-early Permian tectonic-metallogenic framework
%K Southern Paleoasian Domain<br>新疆北部
%K 石炭纪-二叠世构造-成矿事件
%K 古亚洲洋构造域南部
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=80E09230F715381A&yid=37904DC365DD7266&vid=BC12EA701C895178&iid=94C357A881DFC066&sid=D7C79E0E439D0B57&eid=BB5084A31068995F&journal_id=1000-0569&journal_name=岩石学报&referenced_num=64&reference_num=227