ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青岛榴辉岩及胶南群片麻岩的锆石U-Pb年龄──胶南群中晋宁期岩浆事件的证据
  
关键词:magmatic event  U-Pb zircon ages  gneiss of the Jiaonan Group
基金项目:国家自然科学基金
作者单位
李曙光 中国科学技术大学地球与空间科学系 
陈移之 中国科学技术大学地球与空间科学系 
葛宁洁 中国科学技术大学地球与空间科学系 
刘德良 中国科学技术大学地球与空间科学系 
张志敏 山东省地质矿产局区域地质调查队 
张巧大 中国地质科学院地质研究所 
赵敦敏 中国地质科学院地质研究所 
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摘要:
U-Pb ZIRCON AGES OF ECLOGITE AND GNEISS FROMJIAONAN GROUP IN QINGDAO AREAEVIDENCE FOR THE JINNING MAGATIC EVENT INHISTORY OF THE JIAONAN GROUP
      The Jiaonan group developed in the Su-Lu terrain is a basement of sudbucted continental crust onthe northern margin of the Yangtze Block.It is mainly composed of sneisses and a small amount of am-phiholites , marbles ,ultramafic rocks and eclogites, and was considered to De early and middle Protero-zoic rocks in literature. Abundant Sm-Nd and  ̄(40)Ar/ ̄(39)Ar isotopic chronolosy results have demonstratedthat the Jiaonan group complex has been experienced a Triassic high-and ultrahigh-pressure metamor-phism which related to collision between the North China and Yangtze Block. However, there is no reli-able age for their protolithes. This paper reports two U-Pb zircon ages of eclogite and gueiss from theJiaonan group in Qindao area:(1)5 fractions of euhedral zircon from eclogite sive very similar  ̄(206)Pb/ ̄(238)U and  ̄(207)Pb/ ̄(235)U ap-parent ages below the concordia curve,thus can not forming a precise discordia line. Their  ̄(207)Pb/ ̄(206) Pbappareiit ages of 682- 730 Ma perhape cloae to their crystalline age.(2 )5 fractions of euhedral zircons from srieiss give a precise discordia line.Its lower intercept ageof 202 ̄(+12)-14Ma is consistent with the Triassic ultrahigh pressure metamorphic time in this area.Its upperintercept age of 87 ̄+47 ̄(-45)Ma may indicate their crystalline age.Above results suggest that the gneisses in the Jiaonan group are not totally early and middle Pro-terozoic rocks and a part of them are latter Proterozoic plutonic intrusions. The protolith of eclogitefrom the Qingdao area may be a latter Proterozoic island are volcanics. Terefore, the Jinnig movement(700-1 000Ma)should be occurred in the Su-Lu terrain.
LI Shu-guang,CHEN Yi-zhi,GE Ming-jie,LIU De-liang,ZHANG Zhi-min,ZHANG Qiao-da,ZHAO Dun-min.1994.U-Pb ZIRCON AGES OF ECLOGITE AND GNEISS FROMJIAONAN GROUP IN QINGDAO AREAEVIDENCE FOR THE JINNING MAGATIC EVENT INHISTORY OF THE JIAONAN GROUP[J].Acta Geoscientica Sinica,15(1,2):35-36.
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