%0 Journal Article
%T Reply to Comments on "Origin and structural nature of Raobozhai ultamafic rock: A discussion"<br>对“也谈铙钹寨超镁铁岩体的成因和构造类型的归属问题”一文评论的答疑
%A WANG XiBing
%A <br>王希斌
%J 岩石学报
%D 2006
%I 
%X ZHANG Qi's comments argued that the Raobazhai ultramafic body is a mantle metasomatic peridotite rather than an ophiolitie peridotite.Our answer is that metasomatic mantle is not a criterion for discriminating the nuture of mantle rock,because mantle metasomatism may occur both in continental mantle and oceanic mantle.The Raobazhai uhramafic body consists of strongly depleted harzburgite and lherzolite,and some podiform and nodular chromitite ore body.The podiform chromite shows affinities of ophiolitic mantle other than that of continental mantle.The ophiolitic mantle has experienced amphibolite-granulite phase metamorphism.
%K Dabieshan
%K Raobazhai rock body
%K Metamorphism
%K Oceanic lithospheric mantle
%K Continental lithospheric mantle
%K Ophiolite
%K Podiform chromite<br>大别山
%K 铙钹寨岩体
%K 高压变质作用
%K 大洋岩石圈地幔
%K 大陆岩石圈地幔
%K 蛇绿岩
%K 豆荚状铬铁矿
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=7B0296794AD2B594&yid=37904DC365DD7266&vid=BC12EA701C895178&iid=59906B3B2830C2C5&sid=D3F5BDE73FE64227&eid=DCEC7F681FD458B7&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=73