%0 Journal Article
%T THE MAIN CHARACTERISTICS OF THE PALEORIFT IN THE MIDDLE SECTION OF THE TANCHENG--LUJIANC FRACTURE ZONE<br>郯庐断裂中段古裂谷的基本特征
%A XU Zhi-qin
%A ZHANG Qiao-da
%A ZHAO Min
%A <br>许志琴
%A 张巧大
%A 赵民
%J 地球学报
%D 1982
%I 
%X The evidence of the paleorift (J_3-K_2) in the middle section of the Tan-cheng-Lujiang Fracture Zone is described here in detail. A preliminary conc-lusion about the paleorift is obtained through reconstruction of paleotectonicsand paleogeomorphology, elucidation of magmatic evoluttion and deep struct-ures, and comparison with some typical rifts in the world.
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A2604DAA5D2319D4768&yid=3F3D540C9B7906DE&vid=E158A972A605785F&iid=CA4FD0336C81A37A&sid=BCA2697F357F2001&eid=1AE5323881A5ECDC&journal_id=1006-3021&journal_name=地球学报&referenced_num=2&reference_num=0