|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 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 | 华夏南部可能存在Grenville期造山作用:来自基底变质岩中锆石U-Pb定年及Lu-Hf同位素信息显示文摘对华夏地块南部粤中增城和赣南鹤仔3个基底变质岩的地球化学和碎屑锆石年代学研究表明,它们的原岩都是形成于晚新元古代的沉积岩.3个变质沉积岩都主要由新元古代早期(1.0~0.9Ga)的碎屑物质组成,并混有少量中元古代和新元古代中晚期(0.8~0.6Ga)的碎屑物,说明沉积物主要来源于一个遭受过Gondwana大陆聚合事件影响的Grenville期造山带.碎屑锆石的Hf同位素成分显示这些Grenville期锆石可能是造山旋回早期形成的弧与古老大陆碰撞产生的岩浆结晶的.结合华夏地块其他地区~1.0Ga年龄锆石的分布及形态学特征,本文认为华夏地块的南缘很可能曾经存在或者极其靠近一个Grenville期的造山带.而这期造山作用的时代与东印度以及东南极的Grenville造山带一致,且同样受到Gondwana大陆聚合事件的影响.因此,从Rodinia超大陆裂解到Gondwana超大陆聚合期间,华南地块很可能位于澳大利亚西部而与东印度和东南极相邻. | 王丽娟 于津海 O’Reilly S.Y. Griffin W.L. 孙涛 魏震洋 舒良树 蒋少涌 | 2008 | 科学通报2008，53，14： | 52 |
| 3 | 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 |
| 4 | 东准噶尔盆地巴塔玛依内山组火山岩锆石U-Pb年代及Hf同位素研究显示文摘对准噶尔盆地陆梁隆起东部三参1井所钻巴塔玛依内山组玄武岩,开展了详细锆石内部结构研究基础上的U-Pb年代学、微量元素和Hf同位素系统分析.结果显示,所有锆石都属岩浆成因,都有一致的稀土配分型式,都具明显的Ce正异常(δCe=5.06~134)、Eu负异常(δEu=0.06~0.55)和重稀土元素富集特征.25颗锆石中,谐和年龄主要分成3组,分别是(300.4±1.3)Ma(n=11),(339.2±2.7)Ma(n=3)和(392.0±1.7)Ma(n=8);此外,还有3颗近谐和年龄锆石,它们的206Pb/238U年龄分别是(510±7),(488±6)和(453±6)Ma.最小的谐和年龄为(300.4±1.3)Ma,可以代表巴塔玛依内山组火山岩的形成时代(如晚阶段年龄).其他年龄如早泥盆世、奥陶纪等,与盆地周缘岛弧火山岩(富集Pb)和蛇绿岩的时代一致,而且这些年龄锆石都具有正的εHf(t)值(+3.6^+10.5),推测所研究火山岩穿越的盆地基底,可能与由早古生代-中古生代的残余洋壳和岛弧地体组成有关.晚石炭世锆石的εHf(t)值变化于+17.1^+4.2,显示该玄武岩主要来源于软流圈地幔或亏损岩石圈地幔熔融作用,熔体在上升-侵位过程中混染了少量较古老基底物质组分.由于这些玄武岩是后碰撞幔源岩浆直接加入到地壳的物质表现,推测东准噶尔地区晚石炭世已经有了大规模的陆壳垂向生长过程. | 苏玉平 郑建平 Griffin William L 汤华云 O'Reilly Suzanne Y 林向洋 | 2010 | 科学通报2010，55，30： | 50 |
| 5 | Formation history and protolith characteristics of granulite facies metamorphic rock in Central Cathaysia deduced from U-Pb and Lu-Hf isotopic studies of single zircon grains显示文摘The petrochemical as well as zircon U-Pb and Lu-Hf isotopic studies of granulite facies metamorphic rock from the Taoxi Group in eastern Nanling Range, Central Cathaysia indicate that its protolith is the sedimentary rock with low maturation index. The clastic materials are mostly from middle Neoproterozoic (~736 Ma) granitoid rocks with minor Neoarchaean and Paleoproterozoic rocks. The timing of this Neoproterozoic magmatism is in agreement with the second period of magmatism widespread surrounding the Yangtze Block. Hf isotopic data indicate that the Neoproterozoic granitoids resulted from the recycled Paleoproterozoic mantle-derived crustal materials. The sedimentary rock was deposited in Late Neoproterozoic Era, and carried into low crust in Early Paleozoic. The partial melting of the meta-sedimentary rock took place at about 480 Ma and subsequently granulite facies metamorphism occurred at ca. 443 Ma. The zircons forming during this time interval (Early Paleozoic) show large Hf isotope variations, and their -Hf(t) values increase from -13.2 to +2.36 with decreasing age, suggesting the injection of mantle-derived materials during partial melting and metamorphism processes in the Early Paleozoic. Calculation results show that this metamorphic rock, if evolved to Mesozoic, has similar isotopic composition to the nearby Mesozoic high Si peraluminous granites, implying that this kind of granulite facies metamorphic rock is probably the source material of some Mesozoic peraluminous granitoids in eastern Nanling Range. | YU Jinhai ZHOU Xinmin Y. S. O'Reilly ZHAO Lei W. L. Griffin WANG Rucheng WANG Lijuan CHEN Xiaomin | 2005 | Chinese Science Bulletin2005，50，18： | 35 |
| 6 | 华北东部地幔改造作用和置换作用:单斜辉石激光探针研究显示文摘对山东蒙阴古生代金伯利岩中石榴石方辉橄榄岩、河南鹤壁新生代玄武岩中 铬尖晶石方辉橄榄岩、山东栖霞新生代玄武岩中央晶石二辉橄榄岩和山东山旺新生代 玄武岩中尖晶石(富CpX)二辉橄榄岩单斜辉石的常量、微量元素的研究和对比表明:华 北地块古生代稳定存在的克拉通岩石圈地幔在中、新生代其东部被具大洋地幔性质的 显生宙地幔不均匀地发生了置换作用,残存于南北重力梯度带(岩石圈减薄过渡带)上 的鹤壁浅部克拉通地幔除保存有置换作用前改造作用的丰富信息外,也包含有其深部 被置换后的地幔改造作用信息;郯庐断裂带东部栖霞的新生地幔仍保留有较多的大洋 地幔成分特征,而郯庐断裂带内山旺的新生地幔受后续地幔改造作用的影响有向大陆 地幔演化的趋向.发生于华北地块东部中、新生代的岩石圈巨厚减薄作用与地幔的置换 作用有关,由渐进的富CO_2流体或碳酸岩熔体对岩石圈地幔的交代改造作用以及由此 所引起的熔体抽取作用是完成新生地幔对古老地幔置换作用的关键.郯庐断裂带等岩 石圈深大断裂为地幔改造作用和地幔置换作用提供了良好的通道作用. | 郑建平 路凤香 S. Y O’Reilly W. L. Griffin 张明 | 2000 | 中国科学(D辑)2000，30，4： | 27 |
| 7 | Grenvillian orogeny in the Southern Cathaysia Block:Constraints from U-Pb ages and Lu-Hf isotopes in zircon from metamorphic basement显示文摘Metamorphic basement rocks in the Cathaysia Block are composed mainly of meta-sediments with different ages. New zircon U-Pb geochronological results from the meta-sedimentary rocks exposed in the Zengcheng and Hezi areas, southern Cathaysia Block, show that they consist dominantly of early Neoproterozoic (1.0―0.9 Ga) materials with minor Paleo- to Mesoproterozoic and late Neoproterozoic (0.8―0.6 Ga) components, suggesting that the detritus mostly come from a Grenvillian orogen. The youngest detrital zircon ages place a constraint on the deposition time of these sediments in Late Neoproterozoic. Zircon Hf isotopic compositions indicate that the Grenvillian zircons were derived from the reworking of Mesoproterozoic arc magmatic rocks and Paleoproterozoic continental crust, implying an arc-continent collisional setting. Single-peak age spectra and the presence of abundant euhedral Grenvillian zircons suggest that the sedimentary provenance is not far away from the sample location. Thus, the Grenvillian orogen probably preexisted along the southern margin of the Cathaysia Block, or very close to the south. Similarity in the ages of Grenvillian orogeny and the influence of the assembly of Gondwana in South China with India and East Antarctic are discussed, with suggestion that South China was more likely linked with the India-East Antarctica continents in Early Neoproterozoic rather than between western Laurentia and eastern Australia. | WANG LiJuan YU JinHai S.Y. O'REILLY W.L. GRIFFIN SUN Tao WEI ZhenYang JIANG ShaoYong SHU LiangShu | 2008 | Chinese Science Bulletin2008，53，19： | 21 |
| 8 | Zircon U-Pb and Hf isotopes of volcanic rocks from the Batamayineishan Formation in the eastern Junggar Basin显示文摘内部结构的研究被进行从 Batamayineishan 形成调查 U-Pb 年龄,踪迹元素和玄武岩的锆石的 Hf 同位素。暗岩从练习井圣罐头被获得 1 在 Junggar 盆以内在东方 Luliang 上高举。跟踪所有样品是 magmatic 的锆石表演的元素数据,与类似的 REE 模式,包括积极 Ce (Ce=5.06134 ) ,而是否定 Eu (Eu=0.06 ? 0.55 ) 在重稀土元素元素的异例和丰富。在 25 谷物之中,一致年龄被细分进三个组;300.4 整潲祺潧整的年龄? | SU YuPing ZHENG JianPing GRIFFIN William L TANG HuaYun O'REILLY Suzanne Y LIN XiangYang | 2010 | Chinese Science Bulletin2010，55，36： | 21 |
| 9 | U and Th Contents and Th/U Ratios of Zircon in Felsic and Mafic Magmatic Rocks:Improved Zircon-Melt Distribution Coefficients显示文摘U 和 Th 内容和锆石的 Th/U 比率上的高精确的数据获得了使用第二等的离子团 spectrometry 分析从文学被收集了。在花岗石的岩石中的锆石有 350 ppm U, 140 ppm Th,和 Th/U=0.52 的中部的价值;推荐锆石融化分区系数为杜是 81 并且 8.2 为 DTh。在从 mafic 和中间的岩石的锆石,中部的价值是 270 ppm U , 170 ppm Th ,和 Th/U=0.81 ,并且推荐 zirconmelt 分区系数为杜是 169 并且 59 当锆石与melt 在平衡结晶时,为 DTh , magmatic 锆石的 U 和 Th 内容和 Th/U 比率是低的。增加的岩浆温度应该相对 U 内容支持更高的 Th 内容,导致为在到比在花岗石的岩石中的中间的岩石的 mafic 的锆石的更高的 Th/U 比率。然而,当锆石与 melt 在不平衡结晶时, U 和 Th 更容易能进入锆石格子,并且他们的内容和 Th/U 比率主要取决于不平衡的度。在 magmatic 锆石的 U 和 Th 的行为能被用作 geochemical 指示物决定起源和 magmatic 锆石的结晶化环境。 | WANG Xiang Williams L. GRIFFIN CHEN Jie HUANG Pinyun LI Xiang | 2011 | Acta Geologica Sinica(English Edition)2011，85，1： | 18 |
| 10 | 阿尔茨海默病神经细胞凋亡与小胶质细胞活化的关系显示文摘目的 探讨阿尔茨海默病 (Alzheimer′sdisease ,AD)神经细胞凋亡与小胶质细胞活化的关系及活化的小胶质细胞在AD老年斑形成和进展中的作用。方法 收集 10例AD尸检材料及 4例非神经系统疾病死亡的老年尸检材料作为对照 ,进行白细胞介素 1α(IL 1α)免疫组织化学和原位DNA末端转移酶技术 (TUNEL)双重标记及淀粉样 β蛋白免疫组织化学和TUNEL双重标记。 结果 AD组静止的小胶质细胞数与对照组差异无显著性 (P >0 0 5 ) ,但活化的小胶质细胞数明显比对照组高 (P <0 0 1)。活化的小胶质细胞增大、变形 ,可进一步分为初级活化的小胶质细胞、增大的小胶质细胞及巨噬细胞 3种亚型。上述 3种活化的小胶质细胞数分别为 (5 4 0± 0 87)、(11 5 0± 1 2 5 )、(3 4 0± 0 32 )个 /mm2 ,占所有活化的小胶质细胞的比例分别为 2 6 6 0 % ,5 6 6 5 % ,16 75 %。AD组TUNEL阳性的凋亡的神经细胞数明显比对照组高 (P <0 0 5 ) ,且凋亡的神经细胞与活化的小胶质细胞之间具有相关性 (P <0 0 1)。活化的小胶质细胞在 4种类型老年斑中的分布比例不同 ,许多初级活化的小胶质细胞 (4 2 3% ) ,大多数增大的小胶质细胞和巨噬细胞 (分别是 5 6 2 %、70 6 % )分布在弥漫性神经突斑中。结论 小胶质细胞增生。 | 刘冬戈 何淑蓉 张伟 崔娣 Yue kui Li W. Sue T. Griffin | 2004 | 中华病理学杂志2004，33，5： | 17 |
| 11 | 长江中下游溧水盆地中基性次火山岩-侵入岩的锆石U-Pb定年和Lu-Hf同位素显示文摘对溧水盆地8件典型的中生代次火山岩-侵入岩进行了详细的锆石U-Pb年代学和Lu-Hf同位素研究.结果显示,老虎头角闪闪长玢岩年龄为130.5±1.6 Ma,大铜山角闪闪长玢岩年龄为136.0±3.4 Ma,大魏庄角闪闪长玢岩年龄为132.7±2.7 Ma,野山凹粗安斑岩年龄为127.0±1.9 Ma,砚瓦桥石英闪长玢岩年龄为129.4±1.7 Ma,西北山辉石闪长玢岩年龄为133.2±2.1 Ma,长山头黑云母安山玢岩年龄为131.1±2.3 Ma,尖山黑云母粗安斑岩年龄为127.4±1.8 Ma.所有岩浆岩均为早白垩世产物,指示了溧水盆地岩浆活动的峰期时代.岩浆岩的锆石?Hf(t)值变化于-3.54^-9.11,其中大多数变化于-3.54^-5.93,与长江中下游其他火山岩盆地中同时代火山岩和侵入岩的锆石Hf同位素组成相似,表明它们具有相似的源区组成.在分析长江中下游地区以及邻区同时代岩浆特征的基础上,提出俯冲太平洋板块后撤模式来解释中国东部晚中生代岩浆活动.侏罗纪中晚期-白垩纪早期(170~135 Ma),太平洋板块向欧亚大陆俯冲,总体处于挤压背景,岩浆活动呈现出由沿海向内陆年轻化的趋势,且多具壳源特征;白垩纪早期(~135 Ma)之后,太平洋板块的俯冲作用减弱,俯冲板片发生后撤,研究区总体转变为拉张背景,从而形成了一系列火山盆地,造成大量富集地幔和较少量古老地壳物质的熔融,形成大量中基性岩浆岩. | 王丽娟 黄建平 于津海 GRIFFIN W.L. 王汝成 张少琴 杨颍鹤 | 2014 | 科学通报2014，59，14： | 17 |
| 12 | 古老大陆岩石圈地幔再循环与蛇绿岩中铬铁矿床成因显示文摘不同地区、不同时代蛇绿岩中不同类型铬铁矿岩的Re-Os同位素研究表明,在铬铁矿石或围岩中均存在极度亏损的具有大陆岩石圈地幔属性的物质。新疆达拉布特古生代蛇绿岩带中萨尔托海富Al铬铁矿岩的Os同位素组成为0.1109~0.1256,对应的模式年龄为3.5~0.6Ga;西藏班公湖—怒江中生代蛇绿岩带中东巧富Cr铬铁矿石及围岩Os同位素组成介于0.1175~0.1261,对应的模式年龄为1.5~0.1Ga;雅鲁藏布江中生代蛇绿岩带中罗布莎富Cr铬铁矿岩的Os同位素变化范围为0.1038~0.1266,对应的模式年龄为3.37~0.28Ga,而该带中不含矿的泽当二辉橄榄岩的Os同位素组成为0.1256~0.1261,没有古老大陆岩石圈地幔属性的物质存在,与新特提斯洋地幔Os组成较为接近。推测在蛇绿岩形成过程中,古老大陆岩石圈地幔参与循环有利于形成铬铁矿床,明确提出'熔体与古老大陆岩石圈地幔反应成矿'的假说,指出蛇绿岩带中存在的古老微陆块可能是找矿的指示标志。 | 史仁灯 黄启帅 刘德亮 樊帅权 张晓冉 丁林 William L GRIFFIN Suzanne Y O'REILLY | 2012 | 地质论评2012，58，4： | 15 |
| 13 | 西部华夏地区深部可能存在与华北和扬子大陆相似的太古代基底显示文摘华夏地区是否存在古陆是一个长期争论的问题。火山作用的天然超深钻取样,提供了探索大陆基底属性和形成演化过程的重要手段。西部华夏地区地表所出露的最古老岩石不老于中元古代,但对广西省东南部晚中生代—新生代火山岩中锆石捕虏晶的U-Pb年代学和Lu-Hf同位素研究则表明:与华北和扬子大陆相似,西部华夏地区有未暴露的太古代基底。该基底的主体年龄是2.9-2.5Ga,也有3.85Ga,3.55Ga和3.3-3.2Ga的年龄等。它们的亏损地幔模式年龄(tDM)为2.5Ga至≥3.9Ga。说明西部华夏地区的基底经历了复杂的改造过程,包括3.6-3.2Ga,2.5Ga,1.0Ga和0.5Ga时的地幔物质加入,以及2.0-1.8Ga和1.6-1.5Ga时的地壳再熔融事件等。对西部华夏地区强烈改造岩石圈的认识,将有助于从物质组分角度对华南成矿作用背景的思考。华夏地区是否存在古陆是一个长期争论的问题。火山作用的天然超深钻取样,提供了探索大陆基底属性和形成演化过程的重要手段。西部华夏地区地表所出露的最古老岩石不老于中元古代,但对广西省东南部晚中生代—新生代火山岩中锆石捕虏晶的U-Pb年代学和Lu-Hf同位素研究则表明:与华北和扬子大陆相似,西部华夏地区有未暴露的太古代基底。该基底的主体年龄是2.9-2.5Ga,也有3.85Ga,3.55Ga和3.3-3.2Ga的年龄等。它们的亏损地幔模式年龄(tDM)为2.5Ga至≥3.9Ga。说明西部华夏地区的基底经历了复杂的改造过程,包括3.6-3.2Ga,2.5Ga,1.0Ga和0.5Ga时的地幔物质加入,以及2.0-1.8Ga和1.6-1.5Ga时的地壳再熔融事件等。对西部华夏地区强烈改造岩石圈的认识,将有助于从物质组分角度对华南成矿作用背景的思考。 | 郑建平 Griffin WL 汤华云 张志海 苏玉平 刘观亮 | 2008 | 高校地质学报2008，14，4： | 13 |
| 14 | 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 |
| 15 | Prospective randomized controlled trial evaluating cap-assisted colonoscopy vs standard colonoscopy显示文摘AIM: To study the significance of cap-fitted colonoscopy in improving cecal intubation time and polyp detection rate. METHODS: This study was a prospective randomized controlled trial conducted from March 2008 to February 2009 in a tertiary referral hospital at Sydney. The primary end point was cecal intubation time and the secondary endpoint was polyp detection rate. Consecutive cases of total colonoscopy over a 1-year period were recruited. Randomization into either standard colonoscopy (SC) or cap-assisted colonoscopy (CAC) was performed after consent was obtained. For cases randomized to CAC, one of the three sizes of cap was used: D-201-15004 (with a diameter of 15.3 mm), D-201-14304 (14.6 mm) and D-201-12704 (13.0 mm). All of these caps were produced by Olympus Medical Systems, Japan. Independent predictors for faster cecal time and better polyp detection rate were also determined from this study. RESULTS: There were 200 cases in each group. There was no signif icant difference in terms of demographic characteristics between the two groups. CAC, when compared to the SC group, had no signif icant difference in terms of cecal intubation rate (96.0% vs 97.0%, P = 0.40) and time (9.94 ± 7.05 min vs 10.34 ± 6.82 min, P = 0.21), or polyp detection rate (32.8% vs 31.3%, P = 0.75). On the subgroup analysis, there was no significant difference in terms of cecal intubation time by trainees (88.1% vs 84.8%, P = 0.40), ileal intubation rate (82.5% vs 79.0%, P = 0.38) or total colonoscopy time (23.24 ± 13.95 min vs 22.56 ± 9.94 min, P = 0.88). On multivariate analysis, the independent determinants of faster cecal time were consultant-performed procedures (P < 0.001), male patients (P < 0.001), non-usage of hyoscine (P < 0.001) and better bowel preparation (P = 0.01). The determinants of better polyp detection rate were older age (P < 0.001), no history of previous abdominal surgery (P = 0.04), patients not having esophagogastroduodenoscopy in the same setting (P = 0.003), trainee-performed procedures (P = 0.01), usage of hyoscine (P = 0.01) and procedures performed for polyp follow-up (P = 0.01). The limitations of the study were that it was a single-center experience, no blinding was possible, and there were a large number of endoscopists. CONCLUSION: CAC did not signif icantly different from SC in term of cecal intubation time and polyp detection rate. | Hoi-Poh Tee Crispin Corte Hamdan Al-Ghamdi Emilia Prakoso John Darke Raman Chettiar Wassim Rahman Scott Davison Sean P Griffin Warwick S Selby Arthur J Kaffes | 2010 | World Journal of Gastroenterology2010，16，31： | 10 |
| 16 | 华北克拉通西部陆块北缘新生代岩石圈地幔特征的初步研究显示文摘凉城、四子王旗、三义堂和大同的地幔包体的岩石学和矿物的主、微量元素成分显示华北克拉通中、西部北缘总体为过渡型岩石圈地幔,为原始地幔经过不同程度的熔体抽取和后期交代富集作用的残留。凉城岩石圈地幔经历的熔体抽取程度最低,后期交代富集作用比较强烈,这与其橄榄岩中尖晶石的Cr#较低,并且共存的单斜辉石的Mg#较低一致。三义堂岩石圈地幔经历的熔体抽取程度最高,后期交代富集作用最强烈,不同样品甚至同一样品中不同单斜辉石颗粒的La/Yb和LREE配分模式变化范围非常大,且矿物边部比核部更富集微量元素。大同、四子王旗岩石圈地幔经历的熔体抽取程度介于凉城和三义堂之间,但后期的交代富集作用明显不如凉城和三义堂强烈。研究区的岩石圈地幔主要受硅酸盐熔体交代作用的影响,只有三义堂岩石圈地幔还可能也受到了碳酸盐交代作用的影响。 | 王亚妹 William L GRIFFIN 韩宝福 WANG YaMei HAN BaoFu | 2011 | 岩石学报2011，27，10： | 9 |
| 17 | Serological diagnosis of nasopharyngeal carcinoma by enzyme linked immunosorbant assay:optimization,standardization and diagnostic criteria显示文摘Serologicaldiagnosisofnasopharyngealcarcinomabyenzymelinkedimmunosorbantasay:optimization,standardizationanddiagnosticcriteri... | M.H. Ng, H.L. Chen, R.X. Luo, K.H. Chan, P.C.Y. Woo, J.S.T. Sham, J. Huang, W.H.Seto P. Smith and B.E. Griffin | 1998 | Chinese Medical Journal1998，，6： | 8 |
| 18 | Operative complications and economic outcomes of cholecystectomy for acute cholecystitis显示文摘BACKGROUND Recent management of acute cholecystitis favors same admission(SA)or emergent cholecystectomy based on overall shorter hospital stay and therefore cost savings.We adopted the practice of SA cholecystectomy for the treatment of acute cholecystitis at our tertiary care center and wanted to evaluate the economic benefit of this practice.We hypothesized that the existence of complications,particularly among patients with a higher degree of disease severity,during SA cholecystectomy could negate the cost savings.AIM To compare complication rates and hospital costs between SA vs delayed cholecystectomy among patients admitted emergently for acute cholecystitis.METHODS Under an IRB-approved protocol,complications and charges for were obtained for SA,later after conservative management(Delayed),or elective cholecystectomies over an 8.5-year period.Patients were identified using the acute care surgery registry and billing database.Data was retrieved via EMR,operative logs,and Revenue Cycle Operations.The severity of acute cholecystitis was graded according to the Tokyo Guidelines.TG18 categorizes acute cholecystitis by Grades 1,2,and 3 representing mild,moderate,and severe,respectively.Comparisons were analyzed withχ2,Fisher’s exact test,ANOVA,ttests,and logistic regression;significance was set at P<0.05.RESULTS Four hundred eighty-six(87.7%)underwent a SA while 68 patients(12.3%)received Delayed cholecystectomy.Complication rates were increased after SA compared to Delayed cholecystectomy(18.5%vs 4.4%,P=0.004).The complication rates of patients undergoing delayed cholecystectomy was similar to the rate for elective cholecystectomy(7.4%,P=0.35).Mortality rates were 0.6%vs 0%for SA vs Delayed.Patients with moderate disease(Tokyo 2)suffered more complications among SA while none who were delayed experienced a complication(16.1%vs 0.0%,P<0.001).Total hospital charges for SA cholecystectomy were increased compared to a Delayed approach($44500±$59000 vs$35300±$16700,P=0.019).The relative risk of developing a complication was 4.2x[95%confidence interval(CI):1.4-12.9]in the SA vs Delayed groups.Among eight patients(95%CI:5.0-12.3)with acute cholecystitis undergoing SA cholecystectomy,one patient will suffer a complication.CONCLUSION Patients with Tokyo Grade 2 acute cholecystitis had more complications and increased hospital charges when undergoing SA cholecystectomy.This data supports a selective approach to SA cholecystectomy for acute cholecystitis. | Christopher P Rice Krishnamurthy B Vaishnavi Celia Chao Daniel Jupiter August B Schaeffer Whitney R Jenson Lance W Griffin William J Mileski | 2019 | World Journal of Gastroenterology2019，25，48： | 8 |
| 19 | Destabilization of strigolactone receptor DWARF14 by binding of ligand and E3-1igase signaling effector DWARF3显示文摘 | Li-Hua Zhao X Edward Zhou Wei Yi Zhongshan Wu Yue Liu Yanyong Kang Li Hou Parker W de Waal Suling Li Yi Jiang Adrian Scaffidi Gavin R Flematti Steven M Smith Vinh Q Lam Patrick R Griffin YonghongWang Jiayang Li Karsten Melcher H Eric Xu | 2015 | Cell Research2015，25，11： | 7 |
| 20 | Kirigami-inspired,highly stretchable microsupercapacitor patches fabricated by laser conversion and cutting显示文摘The recent developments in material sciences and rational structural designs have advanced the field of compliant and deformable electronics systems.However,many of these systems are limited in either overall stretchability or areal coverage of functional components.Here,we design a construct inspired by Kirigami for highly deformable microsupercapacitor patches with high areal coverages of electrode and electrolyte materials.These patches can be fabricated in simple and efficient steps by laser-assisted graphitic conversion and cutting.Because the Kirigami cuts significantly increase structural compliance,segments in the patches can buckle,rotate,bend and twist to accommodate large overall deformations with only a small strain(<3%)in active electrode areas.Electrochemical testing results have proved that electrical and electrochemical performances are preserved under large deformation,with less than 2%change in capacitance when the patch is elongated to 382.5%of its initial length.The high design flexibility can enable various types of electrical connections among an array of supercapacitors residing in one patch,by using different Kirigami designs. | Renxiao Xu Anton Zverev Aaron Hung Caiwei Shen Lauren Irie Geoffrey Ding Michael Whitmeyer Liangjie Ren Brandon Griffin Jack Melcher Lily Zheng Xining Zang Mohan Sanghadasa Liwei Lin | 2018 | Microsystems & Nanoengineering2018，4，1： | 6 |
您所在的机构暂未开通此部分的功能，请联系管理员