%0 Journal Article
%T Deformation Features and Modeling Experiments of Nappe/Decollement Structure in Xuefeng Mountain Intracontinental Orogenic Belt<br>雪峰山陆内造山带变形特征及挤压推覆—伸展滑脱构造的物理模拟
%A FENG Xiang-yang
%A MENG Xian-gang
%A SHAO Zhao-gang
%A WANG Jian-ping
%A ZHU Da-gang
%A ZHAO Jian-guang
%A <br>冯向阳
%A 孟宪刚
%A 邵兆刚
%A 王建平
%A 朱大岗
%A 赵建光
%J 地球学报
%D 2001
%I 
%X In this paper, the authors have analyzed the deformation features of Xuefeng Mountain intracontinental orogenic belt, and pointed out that Xuefeng Mountain orogenic belt was developed on the basis of the marginal rifted depressive trough of the craton, and experienced Caledonian pre-orogenic epicontinental folding, main orogenic epoch in Indosinian-Yanshanian movement, re-orogenic epoch in late Yanshanian-early Himalayan movement. From Mesozoic, the lithosphere subducted northwestward and the crust was compressed westward. The base surge and nappe were formed and thickened in middle-upper crust. The twin-polarity gravity surge was formed on each side of the orogenic belt during laxity and extension. The model experiment of nappe/decollement structure was done, and the result indicates that the pressure from southeast was the major stress that formed the nappe/decollement structures. The extension structures was formed at the stage of relaxation.
%K intracontinental orogenic belt
%K nappe/decollement structure
%K modeling experiment
%K Xuefeng Mountain<br>陆内造山带
%K 挤压推覆伸展滑脱构造
%K 模拟实验
%K 雪峰山
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A26E10FE0E433C4372B&yid=14E7EF987E4155E6&vid=BC12EA701C895178&iid=94C357A881DFC066&sid=A4E67967A1AB25F0&eid=D1D63D047E37A053&journal_id=1006-3021&journal_name=地球学报&referenced_num=7&reference_num=20