%0 Journal Article
%T Temperature-increase metamorphism along the south boundary of the Dabie eclogite terrain, China.
大别山太湖—马庙断裂带两侧变质地体的增温变质作用
%A Wang Qingchen
%A Cong Bolin
%A Massonne H J
%A
王清晨 Mass.
%A HJ
%J 岩石学报
%D 1999
%I
%X The south boundary of the Dabie eclogite terrain extends west east along Taihu Mamiao faults zone with a south dip Both eclogite and amphibolite along the south of the boundary experienced a temperature increasing and pressure decreasing metamorphic
%K Dabie eclogite terrain
%K South boundary
%K T
%K increase metamorphism
大别山榴辉岩地体
%K 南界
%K 增温变质作用
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=E26616D63CD58443&yid=B914830F5B1D1078&vid=23CCDDCD68FFCC2F&iid=38B194292C032A66&sid=302684F6FB4B24FF&eid=31125890FF093250&journal_id=1000-0569&journal_name=岩石学报&referenced_num=13&reference_num=14