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| 1 | 冀东青龙地区新太古代朱杖子群和单塔子群形成时代:锆石SHRIMP U-Pb定年显示文摘本文报道了冀东青龙地区新太古代朱杖子群和单塔子群变质岩的锆石SHRIMP U-Pb定年结果。朱杖子群底部张家沟组砾岩中的TTG砾石、花岗岩砾石和基质的岩浆锆石207Pb/206Pb加权平均年龄分别为2515±9Ma(MSWD=1.9)、2510±10Ma(MSWD=1.6)和2512±7Ma(MSWD=1.0),朱杖子群底部张家沟组黑云斜长片麻岩碎屑锆石207Pb/206Pb加权平均年龄为2540±6Ma(MSWD=1.6),朱杖子群桲罗台组变质酸性火山岩岩浆锆石207Pb/206Pb加权平均年龄为2516±8Ma(MSWD=1.1),单塔子群鲁杖子组黑云变粒岩碎屑锆石207Pb/206Pb加权平均年龄为2504±7Ma(MSWD=1.8),另有一个数据点的207Pb/206Pb年龄为3.04Ga。根据本文定年结果和前人资料,获得主要结论如下:朱杖子群和单塔子群形成于新太古代晚期,很可能为岛弧环境的产物;朱杖子群与下伏单塔子群之间虽存在角度不整合关系,但时间间断不长,朱杖子群底部张家沟组砾岩不具有底砾岩性质;③绿片岩相—角闪岩相的朱杖子群和单塔子群与角闪岩相—麻粒岩相的遵化深变质绿岩带—三屯营—太平寨—迁安岩浆杂岩区变质程度差异很大,但形成时代相同,是后期构造作用把它们置于同一地壳平面。 | 孙会一 董春艳 颉颃强 王伟 马铭株 刘敦一 Allen NUTMAN 万渝生 | 2010 | 地质论评2010，56，6： | 35 |
| 2 | 中国最老岩石和锆石显示文摘 | 万渝生 刘敦一 董春艳 Nutman A Wilde SA 王伟 颉颃强 殷小艳 周红英 | 2009 | 岩石学报2009，25，8： | 4 |
| 3 | Structural and immunologic cross-reactivity among filarial and mite tropomyosin: Implications for the hygiene hypothesis显示文摘 | Helton C. Santiago Sasisekhar Bennuru Alexis Boyd Mark Eberhard Thomas B. Nutman | 2010 | The Journal of Allergy and Clinical Immunology2010，，2： | 2 |
| 4 | Remnants of ≥3800 Ma crust in the Chinese part of the Sino-Korean Craton显示文摘 | Liu D Y Nutman A P Compston W | 1992 | Geology1992，20，4： | 1 |
| 5 | Testing of some azo dues and their reduction products for mutagenicity using Salmonella typhimurium TA1538显示文摘 | Garner R C Nutman C A | 1977 | Mutation Res1977，，44： | 1 |
| 6 | Remnants of ≥3800 Ma crust in the Chinese part of the Sino-Korean Craton显示文摘 | Liu D Y Nutman A P Compston W Wu,J.S. Shen,Q.H | | 0，，： | 1 |
| 7 | Remants of^3800Ma Crust in the Chinese Part of the Sino-KoreanCraton 显示文摘 | Liu D Y Nutman A P Compston W | 1992 | Geology1992，20，4： | 1 |
| 8 | Remnants of > 3 800 Ma crust in the Chinese part of the Sino-Korean Craton 显示文摘 | Nutman A P Compston W | 1992 | Geology1992，20，： | 1 |
| 9 | The complex age of orthogneiss protoliths exemplified by the Eoarchaean Itsaq Gneiss Complex(Greenland):SHRIMP and old rocks 显示文摘 | HORIE K NUTMAN A P FRIEND C R L | 2010 | Precambrian Research2010，183，1： | 1 |
| 10 | Review of the oldest (4400~3600 Ma) geological and mineralogical record;glimpses of the beginning显示文摘 | Nutman A P Friend C R L Bennett V C | 2001 | Episodes2001，24，： | 1 |
| 11 | Zirconology of the Meeberrie gneiss,Yilgarn Craton,Western Australia:an early Archaean migmatite显示文摘 | Kinny P.D Nutman A.P | | 0，，： | 1 |
| 12 | Reconnaissance dating of events recorded in the southern part of the Capricorn orogen显示文摘 | Kinny P.D Nutman A.P Occhipinti S.A | | 0，，： | 1 |
| 13 | SHRIMP U/Pb zircon ages of acid volcanic rocks in the Chitradurga and Sandur groups and granites adjacent to the Sandur schist belt,Karnataka显示文摘 | Nutman A.P Chadwick B Krishna Rao B Vasudev V.N | | 0，，： | 1 |
| 14 | Remnants of 》3 800 Ma crust in the Chinese part of the Sino-Korean craton显示文摘 | Liu D Y Nutman A P Compston W | 1992 | Geology1992，20，： | 1 |
| 15 | Type 2 cytok- ines and negative immune regulation in human infections显示文摘 | Modlin RL Nutman TB | 1993 | Curr Opin Immunol1993，5，4： | 1 |
| 16 | Iron isotopes may reveal the redox conditions of mantle melting from archean to present显示文摘 | Dauphas N Craddock P R Asimow P D Bennett V C Nutman A P Ohnenstetter D | | 0，，： | 1 |
| 17 | Tyep 2 cytokine and negative immune regulation in human infections显示文摘 | Modlin RL Nutman TB | 1993 | Curr Opin Immunol1993，5，6： | 1 |
| 18 | Remnants of ≥3800 Ma cr ust in theChinese part of the Sino-Korean craton显示文摘 | LIU D Y Nutman A P Compston W | 1992 | Geology1992，20，： | 1 |
| 19 | Strongyloides stercoralis in the immunocom promised population 显示文摘 | Keiser PB Nutman TB | 2004 | Clin Microbiol Rev2004，17，1： | 1 |
| 20 | The Aldan Shield of Siberia, USSR: the age of its Archean components and evidence for widespread reworking in the mid-Proterozoic显示文摘 | Nutman A P Chemyshev I V Baadsgaard H | 1999 | Precambrian Research1999，54，： | 1 |
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