%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