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| 1 | 华北东部橄榄岩与岩石圈减薄中的地幔伸展和侵蚀置换作用显示文摘对比分析了华北不同时代捕虏体橄榄岩及其南部超高压地质体橄榄岩的矿物化学。具古老难熔岩石圈地幔特征的橄榄岩是古生代金伯利岩捕虏体和早中生代苏鲁变质带地质体的主要岩石类型。具这一性质的橄榄岩也构成了河南鹤壁上新世玄武岩捕虏体的主体部分,并可以在辽宁阜新晚中生代玄武岩中被发现。具饱满岩石圈地幔性质的橄榄岩则是阜新晚中生代火山岩、特别是郯庐断裂带(山旺)及其附近地区(栖霞)中新世玄武岩捕虏体的主要类型。从华北东部已有的捕虏体橄榄岩及地质体橄榄岩所表现出的新生饱满与古老难熔地幔的时、空分布特点,即有些地区捕虏体橄榄岩表现出不同性质地幔共存现象(如阜新、鹤壁)或橄榄石Mg#呈渐变关系看:克拉通岩石圈地幔因扬子板块俯冲所引起的早期(如早中生代)地幔伸展、和晚中生代—渐新世因太平洋俯冲所引起的热扰动的软流圈物质上涌对古老地幔产生强烈的侵蚀作用(引起岩石圈的巨大减薄);中新世以来的软流圈热沉降作用出现新生岩石圈地幔并表现为岩石圈的小幅增厚,从而实现地幔置换过程和华北东部岩石圈的整体减薄过程。岩石圈幔内薄弱带及岩石圈深断裂(如郯庐断裂带)起了软流圈物质侵蚀古老岩石圈地幔的通道作用并导引着深部物质运移和不规则减薄作用等。个别地区(如阜新)强烈的软流圈上涌于晚中生代就已经开始,显示地幔置换作用的强烈不均一性。 | 郑建平 路凤香 W L GRIFFIN 余淳梅 张瑞生 袁晓萍 吴秀玲 | 2006 | 地学前缘2006，13，2： | 60 |
| 2 | Finding of ancient materials in Cathaysia and implication for the formation of Precambrian crust显示文摘在 Nanxiongarea 从帕拉片麻岩为 56 由岩屑形成的锆石标明日期的 U-Pb,北广东省,显示在 Cathaysiahinterland 的最近的 Neoproterozoic 沉积由众多的 Grenvillian 和 Neoarchaean 组成碎屑状的材料,以及 someMesoproterozoic 岩屑。次要的 Paleoarchaean (3.76 Ga ) 和 Mesoarchaean (3.0—3.2 Ga ) 锆石,是在华南的最旧的锆石,第一也在沉积被发现,建议卡赛西亚·布洛克可以包含很旧的材料。thirty-sevenzircons 的 Hf 同位素作文表明这些碎屑状的材料有不同起源。次要的锆石从产生从的岩浆结晶相对少年外壳,当大多数锆石的父母岩浆从古老的外壳被导出时。U-Pb 标明日期和这些锆石的 Hf 同位素分析的集成建议在 Cathaysia 块的少年外壳的产生主要发生在 2.5 点—2.6Ga。Mesoarchaean (3.0—3.3 Ga ) ,迟了的 Paleoproterozoic (~ 1 .8 Ga ) 和 Paleoarchaean (~ 3 .7 Ga ) 可以也是外壳的生长的重要事件。Grenvillian magmatism 是极其强烈的,但是它主要涉及与少年外壳的很少形成古老的外壳的部件再循环。~ 2 .1 Ga Hf 模型年龄的 Themarked 存在和有结晶化的锆石的缺席在~ 2 .1 Ga 变老建议许多锆石的父母岩浆可能从由 Neoarchaean 和迟了的 Paleoproterozoic 材料组成的混合来源被导出。 | YU JinHai Y S O'REILLY WANG LiJuan W L GRIFFIN JIANG ShaoYong WANG RuCheng XU XiSheng | 2007 | Chinese Science Bulletin2007，52，1： | 47 |
| 3 | In situ Re-Os isotope ages of sulfides in Hannuoba peridotitic xenoliths: Significance for the frequently-occurring mantle events beneath the North China Block显示文摘In situ Re-Os isotopes of sulfides in peridotitic xenoliths from Cenozoic Hannuoba basalts were analyzed by LAM-MC-ICPMS. The suifides developed two types of occurrences including silicate-enclosed and interstitial. In the enclosed sulfides, 187Os/188Os vary from 0.1124 to 0.1362 and 187Re/188Os from 0.0026 to 1.8027. In the interstitial ones, 187Os/188Os have a range from 0.1174 to 0.1354 and 187Re/188Os from 0.0365 to 1.4469. The oldest age, calculated by TRD for the enclosed sulfides, is 2.1 Ga. An isochron age of 2.3±1.2 Ga is obtained by five grains of enclosed sulfides and primitive mantle. The sulfides used have lower Re-Os isotopic ratio than primitive mantle. Meanwhile, an isochron age of 645±225 Ma is given by all in- terstitial sulfides and the enclosed sulfides with higher Re-Os isotopic ratio due to Re addition after man- tle formation. In addition, the model age of 1.3 Ga recorded by one interstitial sulfide, having similar TDM and TRD, should be meaningful to deep thermal event. The coexistence of different ages, revealed by in situ Re-Os isotope, indicates frequently-occurring mantle events beneath Hannuoba area. | YU ChunMei ZHENG JianPing GRIFFIN W L | 2007 | Chinese Science Bulletin2007，52，20： | 10 |
| 4 | Non-chondritic distribution of the highly siderophile elements in mantle sulfides显示文摘 | Alard O Griffin W L Lorand J P | 2000 | Nature2000，，407： | 1 |
| 5 | Continental growth in the Phanerozoic:Evidence from Central Asia显示文摘 | Jahn B M Griffin W L Windley B F | 2000 | Tectonophysics2000，328，： | 1 |
| 6 | The applica- tion of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology显示文摘 | Jackson S E Pearson N J Griffin W L | 2004 | Chemical Geology2004，211，1： | 1 |
| 7 | Widespread Archean basement beneath the Yangtze eraton 显示文摘 | ZHENG J P GRIFFIN W L O' REILLY S Y | 2006 | Geology2006，7，： | 1 |
| 8 | CD4 ( +)T-cell ac-tivation and induction of autoimmune hepatitis following trichloroethylene treatment in MRL + 1+ mice显示文摘 | Griffin J M Gilbert K M Lamps L W | 2000 | Toxicol Sci2000，57，2： | 1 |
| 9 | Geochemistry and origin of sulphide minerals in mantle xenoliths: Qilin, Southeastern China显示文摘 | Guo J Griffin W L O'Reilly S Y | 1999 | Journal of Petrology1999，40，7： | 1 |
| 10 | The Hf isotopecompositon of cratonic mantle: LA-MC-ICPMS analysis of zir-con megacrysts in kimberlites显示文摘 | Griffin W L Pearson N J * Belousova E A | 2000 | Geochemica et CosmochimicaActa2000，64，： | 1 |
| 11 | Neoproterozoic re- cycling of the Sveconorwegian orogenic belt: Detrital-zircon data from the Sparagmite basins in the Scandinavian Cale- donides 显示文摘 | Bingen B Belousova E A Griffin W L | 2011 | Precambrian Research2011，189，： | 1 |
| 12 | Human nutrition, the gut microbiome and the immune system显示文摘 | KAU A L AHEM P P GRIFFIN N W | 2011 | Nature2011，474，7351： | 1 |
| 13 | The Siberian Lithosphere Traverse: Mantle Terranes and the Assembly of the Siberian Craton显示文摘 | GRIFFIN W L RYAN C G KAMINSKY F V | 1999 | Tectono- physics1999，310，1234： | 1 |
| 14 | Trace elements in sulfide inclusions from Yakutian diamonds显示文摘 | Bulanova G P Griffin W L Ryan C G | 1996 | Contributions to Mineralogy and Petrology1996，124，2： | 1 |
| 15 | Zircon chemistry andmagma mixing, SE China: In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes显示文摘 | Griffin W L Wang X Jackson S E | 2002 | Lithos2002，61，34： | 1 |
| 16 | The application of Ia- set ablation-inductively coupled plasma-mass spectrometry to in si- tu U-Pb zircon geochronology显示文摘 | Jackson S E Pearson N J Griffin W L | 2004 | Chemical Geology2004，211，： | 1 |
| 17 | Precambrian crustalevolution of the Yangtze Block tracked by detrital zircons fromNeoproterozoic sedimentary rocks 显示文摘 | Wang L J W L Griffin Jin Haiyu | 2010 | Precambrian Research2010，177，： | 1 |
| 18 | Detection of channel cat- fish virus DNA in acutely infected channel catfish, Ictalurus punc- tatus (Rafinesque) , using the polymerase chain reaction 显示文摘 | Gray W L Williams R J Griffin B R | 1999 | J Fish Dis1999，22，2： | 1 |
| 19 | Decoupling of U- Pb and Lu- Hf isotopes and trace elements in zircon from the UHP North Qaidam orogen, NE Tibet (China): Tracing the deep subduction of continental blocks显示文摘 | Xiong Q Zheng J P Griffin W L | 2012 | Lithos2012，155，： | 1 |
| 20 | The Hf isotope composition of cratonic mantle: LAM- MC-ICPMS analysis of zircon megacrysts in kimberlites 显示文摘 | GRIFFIN W L PEARSON N J BELOUSOVA E A | 2000 | Geochim Cosmochim Acta2000，64，： | 1 |
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