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| 1 | The role of whole brain radiation therapy in the management of newly diagnosed brain metastases: a systematic review and evidence-based clinical practice guideline显示文摘 | Gaspar LE Mehta MP Patchell RA Burri SH Robinson PD Morris RE Ammirati M Andrews DW Asher AL Cobbs CS Kondziolka D Linskey ME Loeffler JS McDermott M Mikkelsen T Olson JJ Paleologos NA Ryken TC Kalkanis SN. | 2010 | 中国神经肿瘤杂志2010，8，1： | 98 |
| 2 | 北祁连山西段熬油沟蛇绿岩SHRIMP分析结果及其地质意义显示文摘本文通过对北祁连山西段熬油沟蛇绿岩中辉绿岩岩墙中的锆石 SHRIMP法年龄的测定 ,确定出熬油沟蛇绿岩形成于中元古代早期 (约 1777Ma) ,这是迄今为止我国发现的最古老的蛇绿岩。该年龄测定的结果还暗示了本区在 146 6 Ma和5 0 7Ma各有一次地质事件 ,前者可能代表了中元古代早期的洋盆闭合的下限年龄 ,后者代表一次加里东期区域变质事件 ,并且本区可能还存在未出露的新太古代结晶基底 (2 5 6 1Ma)。 | 张招崇 周美付 Paul T ROBINSON 毛景文 杨建民 左国朝 | 2001 | 岩石学报2001，17，2： | 42 |
| 3 | 都兰花岗岩锆石SHRIMP定年及柴北缘超高压带花岗岩年代学格架显示文摘柴北缘超高压带东端都兰地区花岗岩锆石SHRIMP U-Pb定年结果表明,野马滩东岩体的年龄为(406.6±3.5)Ma,巴立给哈滩西岩体的年龄分别为(407.3±4.3)和(397±6)Ma,水文站北岩体的年龄分别为(404.5±4.0)和(397.0±3.7)Ma,水文站南岩体的年龄为(380.5±5.0)Ma,察察公麻岩体的年龄分别为(382.5±3.6)和(372.5±2.8)Ma.从年龄上看,这些花岗岩明显地分为两期:早期的为407-397 Ma,晚期的为383-373 Ma.它们主要为准铝质-弱过铝质的石英闪长岩、花岗闪长岩和二长花岗岩.岩石地球化学研究表明,大多数样品为钙碱性系列,少数样品为钙性或碱钙性系列,其中,早期花岗岩的87Sr/86Sr比值(0.7082-0.7110)和模式年龄(T2DM=1.41-1.90 Ga)高于晚期花岗岩(0.7072-0.7091,T2DM=1.07-1.38 Ga),但晚期花岗岩的εNd(t)值(0.6- -3.0)高于早期花岗岩(-3.2- -9.3),表明早期花岗岩可能起源于早中元古代的大陆壳;而晚期花岗岩起源于晚中元古代玄武质地壳.结合区域地质构造特征,可以认为,早期花岗岩的形成与俯冲板块的断离并折返有关,而晚期花岗岩的形成与造山带岩石圈地幔拆沉作用有关. | 吴才来 郜源红 李兆丽 雷敏 秦海鹏 李名则 刘春花 Ronald B FROST Paul T ROBINSON Joseph L WOODEN | 2014 | 中国科学:地球科学2014，44，10： | 27 |
| 4 | Dur’ngoi Ophiolite in East Kunlun, Northeast Tibetan Plateau: Evidence for Paleo-Tethyan Suture in Northwest China显示文摘The A’nyemaqen (阿尼玛卿) ophiolite belt along the southern margin of the East Kunlun (昆仑) Mountains marks the suture formed by the closure of paleo-Tethys. The Dur’ngoi ophiolite in the eastern part of this belt consists of meta-peridotite, mafic-ultramafic cumulates, sheeted dikes and basaltic lavas. The meta-peridotites consist of dunite, harzburgite, lherzolite, feldspar-bearing lherzolite and garnet-bearing lherzolite and contain residual spinel with Cr# [100×Cr/(Cr+Al)] ranging from 30 to 57 and Mg# [100×Mg/(Mg+Fe2+)] ranging from 50 to 75, indicating an Aland Mg-rich series. The meta-peridotites have a relatively narrow range of composition with Mg# of 89.2–92.6, Al2O3 contents of (1–4) wt.% and slightly depleted chondrite normalized REE patterns, indicating that they represent relict mantle material that has undergone intermediate to low degrees of partial melting. Garnets in the lherzolite are andradite, enriched in Ca and Fe and depleted in Mg and Al (And=95–97, Pyr=0.3–5, Gro=0–3), indicating a metamorphic origin. The cumulate rocks mainly consist of dunite, wehrlite, pyroxenite and gabbro. A well-layered gabbro-pyroxenite complex is defined by modal variations in plagioclase and pyroxene. Blocks of garnet-pyroxenite or rodingite are locally present in the meta-peridotites. Garnets in the cumulate rocks are grossular (Gro=69–90, And=9–19, Br=1–12), also metamorphic origin. The diabase dikes are moderately depleted in LREE [(La/Sm)N=0.5–0.8] and HREE resulting in slightly convex chondrite-normalized patterns with slightly positive Eu anomalies (δEu=1.1–1.3). The basaltic lavas have REE patterns similar to those of MORB with (La/Sm)N ratios of 0.5–1 and small negative Eu anomalies. They appear to have been derived from a depleted mantle source and to have undergone little or no differentiation during crystallization. SHRIMP U-Pb dating of zircons from the basalts yields 206Pb/238U ages of 276–319 Ma (average 308.0±4.9 Ma). The Dur’ngoi ophiolite is interpreted as a dismembered fragment of paleo-oceanic crust emplaced during closure of the paleo-Tethyan Ocean basin. Three other suites of oceanic lavas are recognized in the area: island arc volcanic (IAV) rocks, possible back arc basin (BAB) basalts and possible post-collisional volcanic (PCV) and plutonic rocks. The distribution of these rocks suggests north-directed subduction. Opening of the A’nyemaqen oceanic basin started at least as early as Late Carboniferous (308 Ma) and the basin probably closed during the Early Triassic. The IAV formed in Late Permian (260 Ma), the BAB in Early–Middle Triassic, and the PCV in Late Triassic. Several large scale, ductile, sinistral strike-slip fault zones, extending hundreds to thousands kilometers, formed along or north of the suture during the Early–Late Triassic, e.g., they are the south margin fault zone of East Kunlun (200–220 Ma), the Altyn Tagh fault (220–230 Ma), and the North Qaidam fault zone (240–250 Ma). These strike-slip faults were probably generated by oblique subduction and closure of the paleo-Tethyan Ocean basin, possibly during exhumation of the subducted plate or uplift of the overriding plate, coincident with post-collisional magmatism. | 杨经绥 史仁灯 吴才来 王希斌 Paul T Robinson | 2009 | Journal of China University of Geosciences2009，20，2： | 26 |
| 5 | Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP belt, NW China显示文摘Zircon SHRIMP dating of granites from Dulan,east segment of North Qaidam UHP belt shows that they are 406.6±3.5 Ma for Yematan-E,407.3±4.3 and 397±6 Ma for Balijiehatan-W,404.5±4.0 and 397.0±3.7 Ma for Shuiwenzhan-N,380.5±5.0 Ma for Shuiwenzhan-S,382.5±3.6 and 372.5±2.8 Ma for Chachagongma.These granites from Dulan represent the products of the third and fourth periods of Paleozoic magmatism in North Qaidam.Geochemically,the granitoids with metalumious to weak peratuminous are quartz diorite,granodiorite,and granite in composition and mainly belong to calc-alkaline series,a few samples to calc or alkali-calc series.The third period of granites is a rock association of granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7082 to 0.7110 and T2DM model ages from 1.41–1.90 Ga;and the fourth period of granites is a rock association of quartz diorite+granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7072 to 0.7091 and T2DM model ages from 1.07–1.38 Ga.Therefore,the third period of granites has higher initial 87Sr/86Sr ratios and T2DM model ages.On the contrary,the fourth period of granites has Nd(t)values from 0.6 to-3.0,higher than that of the third granite with Nd(t)values-3.2 to-9.3.Thus,the data comparison indicates that the third granites may derive from Paleo-proterzoic continental crust with mantle material whereas the fourth granites may derive from the Meso-proterzoic basalt crust with continental material.Combined with regional geology,we thought that the third granites were formed relative to plate exhumation and the fourth granites to delamination of the lithospheric mantle. | WU CaiLai GAO YuanHong LI ZhaoLi LEI Min QIN HaiPeng LI MinZe LIU ChunHua Ronald B FROST Paul T ROBINSON Joseph L WOODEN | 2014 | Science China Earth Sciences2014，57，12： | 21 |
| 6 | GPS(全球定位系统)同步电流差动保护的应用显示文摘介绍数字式电流差动保护在输配电网络中作为主保护的应用情况。讨论电力部门为降低成本而租用电信通道时遇到的问题,分析说明GPS同步数字式电流差动保护如何通过同步数字级(SDH或SONET环)电信网而实现保护的高可靠性。 | S H Richards, S Potts, N Robinson, S Pickering, A Apostolov(Alstom T&D Protection & Control, France) | 2002 | 国际电力2002，6，3： | 8 |
| 7 | Studies on the production of enzymes by white rot fungi for the decolourisation of textile dyes 显示文摘 | ROBINSON T CHANDRAN B NIGAM P | 2001 | Enzyme and Microbial Technol2001，29，： | 2 |
| 8 | Foreword显示文摘The Chinese Geophysical Society and China University of Geosciences (CUG) hosted the last three International Conferences on Environmental and En-gineering Geophysics (ICEEG) on the campus of CUG in Wuhan, China, biannually from 2004 to 2008. | 杨经绥 李海兵 Paul T Robinson | 2009 | Journal of China University of Geosciences2009，20，2： | 2 |
| 9 | Transpalatal advancement pharyngoplasty outcomes compared with uvulopalatopharygoplasty显示文摘 | WOODSON B T ROBINSON S LIM H J | 2005 | Otolaryngol Head NeckSurg2005，133，： | 1 |
| 10 | Condensed tannin biosynthesis genes are regulated separately from other flavonoid biosynthesis genes in apple fruit skin显示文摘 | Adam M T Benjamin E U Robinson S P | 2006 | Plant Science2006，170，： | 1 |
| 11 | Early neurological deterioration in acute iscbemic stroke : predictors, mechanisms and management 显示文摘 | Thanvi B Treadwell S Robinson T | 2008 | Postgrad Med J2008，84，： | 1 |
| 12 | Oral and parenteral vaccination against Trichinella spiralis infections in high - and low - responder mice 显示文摘 | Robinson K Bellaby T Wakelin D | 1995 | Int J Parasitol1995，25，8： | 1 |
| 13 | High-chromium and high-alu minum podiform chromitites,western china:relationship to partial melting and melt/rock interaction in the upper mantle 显示文摘 | Zhou M F Robinson P T | 1994 | Intel Geol Rev1994，36，： | 1 |
| 14 | Aeroelastic analysis of wings using the Euler equations with a deforming mesh 显示文摘 | Robinson B A Batina J T Yang H T Y | 1991 | Journal of Aircraft1991，28，11： | 1 |
| 15 | Reference Revitalization and Roving Reference: Are the Reference Desk and Print Reference Sources Pass e ?显示文摘 | Robinson T Triplett B Lambert L | 2011 | The Christian Librarian2011，，2： | 1 |
| 16 | Analytical formulation for the shielding effectiveness of enclosures with apertures显示文摘 | Robinson M P Benson T M Christopoulos C | 1998 | IEEE Trans on Electromagn Compat1998，40，3： | 1 |
| 17 | Effects of supplemental ruminally degradable pro- tein versus increasing amounts of supplemental rumi- nally undegradable protein on nitrogen retention, ap- parent digestibility, and nutrient flux across visceral tissues in lambs fed low-quality forage 显示文摘 | ATKINSON R L TOONE C D ROBINSON T J | 2007 | Journal of Animal Science2007，85，12： | 1 |
| 18 | A temporal link between the Emeishan large igneous province (SW China) and the end-Guagalupian mass extinction 显示文摘 | Zhou M F Malpas J Song X Y Robinson P T Sun M Kennedy A K Lesher C M Keays R R | 2002 | Earth arut Planetary Science Letters2002，196，： | 1 |
| 19 | Meta-analysis of comparison of effectiv-eness of lowering apolipoprotein B ver- sus low-density lipoprotein cholesterol and non high-density lipoprotein cholesterol for cardiovascular risk reduction in randomized trims 显示文摘 | ROBINSON J G WANG S JACOBSON T A | 2012 | Am J Cardiol2012，110，10： | 1 |
| 20 | Simultaneous nitrogen doping and reduction of graphene oxide显示文摘 | LI Xiao-li WANG Hai-liang ROBINSON T Joshua | 2009 | Journal of the Amerkan Chemical Society2009，131，15： | 1 |
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