%0 Journal Article
%T Evidence of spinel fades partial melting of the mantle rocks from the CCSD-PP3 drilling cores<br>中国大陆科学钻探CCSD-PP3钻孔地幔岩的尖晶石相部分熔融证据
%A CHEN ShiZhong
%A YANG JingSui
%A ZHANG ZhongMing
%A <br>陈世忠[
%A ] 杨经绥 张仲明
%J 岩石学报
%D 2006
%I 
%X The mantle rocks from the CCSD PP3 drilling cores in the Sulu UHPM belt are characterized by high contents of Mg and low A1 and Ca,suggesting a much highly depleted mantle rocks than those in the east of China.Geochemical,mineralogical and Re-Os isotope data indicate that the mantle rocks in PP3 were originated from early Proterozoic lithospheric mantle and partial melted at shallow depth under spinel facies during medium-late Proterozoic time.The spinel facies peridotites were transformed into garnet facies peridotites,due to the deep subduction during the collision between the Yangtze and the North China blocks.
%K Garnet peridotites
%K Spinel facies
%K Partial melting<br>石榴橄榄岩
%K 尖晶石相
%K 部分熔融
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=FB830B575C18635E&yid=37904DC365DD7266&vid=BC12EA701C895178&iid=708DD6B15D2464E8&sid=B55917F5071FEB5E&eid=8026A4A06EF64621&journal_id=1000-0569&journal_name=岩石学报&referenced_num=1&reference_num=44