%0 Journal Article
%T Recognition of Neoproterozoic Post-Orogenic Aluminous A-type Granite in Zhuji, Zhejiang Province<br>浙江诸暨新元古代后造山铝质A型花岗岩的厘定
%A ZHOU Yu-zhang
%A XING Guang-fu
%A YANG Zhu-liang
%A SHEn Jia-lin
%A CHEN Rong
%A BAO Chao-min
%A WEI Nai-yi
%A <br>周宇章
%A 邢光福
%A 杨祝良
%A 沈加林
%A 陈荣
%A 包超民
%A 魏乃颐
%J 地球学报
%D 2006
%I 
%X The Neoproterozoic bimodal intrusive association in Daolinshan area of Zhuji consists of moyite and diabase. Based on its field characteristics as well as dating and petrologic features, the authors hold that the granite belongs to the aluminous type. Furthermore, it is confirmed that the granite is of the typical post-orogenic A-type (A2 or PA type). The single zircon age is 816Ma, which suggests that the granite is the earliest A-type granite ever found in South China, and that the breakup of the Supercontinent Rodinia was strong at that time. In view of the main breakup period (825 Ma), it is considered that South China was the center of the breakup of Supercontinent Rodinia.
%K Rodinia
%K post-orogenic A-type granite
%K bimodal intrusive rocks
%K Neoproterozoic
%K Zhuji Zhejiang Province<br>Rodinia
%K 后造山A型花岗岩
%K 双峰式侵入岩
%K 新元古代
%K 浙江诸暨
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=82E53A58B96F5AAB8888092A1D2A353A&yid=37904DC365DD7266&vid=DB817633AA4F79B9&iid=0B39A22176CE99FB&sid=D767283A3B658885&eid=A63576421B012172&journal_id=1006-3021&journal_name=地球学报&referenced_num=4&reference_num=24