DISCOVERY OF THE COESITE-BEARING GRANULITE IN WEIHAI, SHANDONG PROVINCE, CHINA 被引量：1

DISCOVERY OF THE COESITE-BEARING GRANULITE IN WEIHAI, SHANDONG PROVINCE, CHINA

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摘要 With the continuing discoveries of coesite-bearing eclogite, the Dabie Mountainsnorthern Jiangsu-Eastern Shandong ultrahigh pressure metamorphic zone has become a hot spot to international geoscientists. So far, however, eclogites with real coesite were found on-

作者从柏林王清晨张儒媛翟明国赵中岩李家驹

机构地区 Institute of Geology

出处《Chinese Science Bulletin》 SCIE EI CAS 1992年第17期1494-1495,共2页

基金 Project supported by the National Natural Science Foundation of China.

关键词 Jiangsu Shandong METAMORPHIC CONTINUING ultrahigh quartz EASTERN EASTERN GARNET proportion

分类号 N [自然科学总论]

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1徐树桐,苏文,刘贻灿,江来利,季寿元,A.I.OKAY,A.M.C.SENGOR.DIAMONDS FROM HIGH-PRESSURE METAMORPHIC ROCKS IN EASTERN DABIE MOUNTAIN[J].Chinese Science Bulletin,1992,37(2):140-145. 被引量：3
2王晓燕,崔文元,刘树忠,张立飞,魏春景.豫南地区含柯石英榴辉岩的发现[J].岩石学报,1993,9(2):181-185. 被引量：21
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4张泽明,游振东,韩郁菁,桑隆康.大别-苏鲁榴辉岩带的岩石学、变质作用过程及成因研究[J].地质学报,1995,69(4):306-325. 被引量：81
5Jiang Laili,Xu Shutong,Liu Yican,Wu Weiping,Su Wen. The white schist assemblage in the kyanite quartzite from the ultrahigh-pressure metamorphic belt, eastern Dabie Mountains[J] 1998,Chinese Science Bulletin(19):1651～1655
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引证文献1

1徐树桐,刘贻灿,江来利,苏文,吴维平.Confirmation of the ultrahigh-pressure metamorphic belt in the Dabie Mountains and related problems[J].Progress in Natural Science:Materials International,1999,9(1):16-24. 被引量：1

二级引证文献1

1XUShutong,LIUYican,CHENGuanbao,RobertoCompagnoni,FrancoRolfo,HEMouchun,LIUHuifang.New finding of microdiamonds in eclogites from Dabie-Sulu region in central-eastern China[J].Chinese Science Bulletin,2003,48(10):988-994. 被引量：50

1李曙光,刘德良,陈移之,葛宁洁,张宗清,叶笑江.THE Sm-Nd ISOTOPIC AGE OF COESITE-BEARING ECLOGITE FROM THE SOUTHERN DABIE MOUNTAINS[J].Chinese Science Bulletin,1992,37(19):1638-1641. 被引量：8
2徐树桐,刘贻灿,江来利,苏文,吴维平.Confirmation of the ultrahigh-pressure metamorphic belt in the Dabie Mountains and related problems[J].Progress in Natural Science:Materials International,1999,9(1):16-24. 被引量：1
3陈道公,杨杰东,王银喜.NEODYMIUM ISOTOPIC COMPOSITION AND SIGNIFICANCE OF SOME CENOZOIC VOLCANIC ROCKS FROM JIANGSU, ANHUI AND SHANDONG, CHINA[J].Chinese Science Bulletin,1991,36(10):843-846.
4LI Guojun(Department of Mathematics,Yantai Teacher’s College,Yantai 264000,Shandong)LIU Zhenhong(Institute of Systems Science,Academia Sinica,Beijing 100080).Two Sufficient Conditions for Hamiltonian Graphs[J].Systems Science and Systems Engineering,1994,4(1):62-65.
5CHINESE SCIENCE BULLETIN (KEXUE TONGBAO) SUBJECT INDEX TO VOLUME 37(1992)[J].Chinese Science Bulletin,1992,37(24):2094-2112.
6CAO MingHe TIAN Wei LI MingFa SUN WenHua HU MingJi LIU HanXing.Synthesis and structure of NaNbO_3 ceramic powders in ultrahigh pressure field[J].Science China(Technological Sciences),2007,50(5):658-663.
7Shandong University Human Rights Research Center[J].The Journal of Human Rights,2014,13(4):27-31.
8HOU Zhenhui1, LI Shuguang1, CHEN Nengsong2, LI Qiuli1 & LIU Xiaoming3 1. School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China,2. The Key Laboratory of Continental Dynamics of the Ministry of Education, Northwest University, Xi’an 710069, China,3. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China.Sm-Nd and zircon SHRIMP U-Pb dating of Huilanshan mafic granulite in the Dabie Mountains and its zircon trace element geochemistry[J].Science China Earth Sciences,2005,48(12):2081-2091. 被引量：10
9FAN Jin BAO Zhengqiang ZHENG Qingwu ZHOU Zhongming Yangzhou Univ., Yangzhou, 225009 LIU Yaojun Zhengzhou Text. Inst., Zhengzhou, 450007.An Empirical Analysis on Diversity of Regional Economic Growth in Jiangsu Province of China[J].Systems Science and Systems Engineering,1998,8(3):83-90.
10INTRODUCTION TO THE STATE KEY LABORATORY OF CRYSTAL MATERIALS,SHANDONG UNIVERSITY[J].Progress in Natural Science:Materials International,1992,2(4):374-380.

Chinese Science Bulletin

1992年第17期

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DISCOVERY OF THE COESITE-BEARING GRANULITE IN WEIHAI, SHANDONG PROVINCE, CHINA 被引量：1

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