|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | The characteristics, origins, and geodynamic settings of supergiant gold metallogenic provinces显示文摘There are six distinct classes of gold deposits, each represented by metallogenic provinces, having 100’s to > 1 000 tonne gold production. The deposit classes are: (1) erogenic gold; (2) Carlin and Carlin-like gold deposits; (3) epithermal gold-silver deposits; (4) copper-gold porphyry deposits; (5) iron-oxide copper-gold deposits; and (6) gold-rich volcanic hosted massive sul-fide (VMS) to sedimentary exhalative (SEDEX) deposits. This classification is based on ore and alteration mineral assemblages; ore and alteration metal budgets; ore fluid pressure(s) and compositions; crustal depth or depth ranges of formation; relationship to structures and/or magmatic intrusions at a variety of scales; and relationship to the P-T-t evolution of the host terrane. These classes reflect distinct geodynamic settings. Orogenic gold deposits are generated at mid-crustal (4-16 km) levels proximal to terrane boundaries, in transpressional subduction-accretion complexes of Cordilleran style erogenic belts; other | Robert Kerrich Richard Goldfarb David Groves Steven Garwin | 2000 | Science China Earth Sciences2000，43，S1： | 249 |
| 2 | 水-岩-气相互作用引起的水化学动态变化研究——以桂林岩溶试验场为例显示文摘利用多参数自动记录仪对桂林岩溶试验场的降水量、水位、水温、pH值和电导率进行了监测,数据采集间隔根据参数变化的程度由2min到1h不等。结果发现,岩溶裂隙水在洪水期间pH值呈降低趋势,而电导率呈升高的不寻常变化。与此相反,对于岩溶管道水,同样是在洪水期间,它的pH值是升高的,而电导率呈正常的降低。考虑到Ca2+和HCO-3分别为地下水中主要的阴阳离子(>90%),及它们与电导率的线性关系,计算得到了洪水期间方解石的饱和指数(SIc)和水的CO2分压(Pco2)的变化情况。发现洪水时裂隙水的Pco2高于正常情况的Pco2,而它的SIc值比正常情况低。与此相对,对于管道水,尽管同一洪水期间其SIc降低,但Pco2也降低。从这些结果,可以推断,至少有两个关键的过程控制着洪水期间的水化学变化。一个是雨水的稀释作用,另一个是水-岩-气的相互作用。然而,对于裂隙水来说,后者的作用可能更重要,即在洪水期间,高浓度的土壤CO2溶解于水中,则更具侵蚀性的水能溶解更多的石灰岩,从而增强水的电导率。而对于管道水,雨水的稀释作用更重要,因为研究区较高的pH和低电导率的雨水能更快地通过管道流出,所以,要了解岩溶系统水化学的变化,仅考虑水-岩相互作用是不够的,我们还必须重视CO2气体对岩溶系统中水化学变化的影响。总之。 | 刘再华 Chris GROVES 袁道先 Joe MEIMAN 姜光辉 何师意 | 2003 | 水文地质工程地质2003，30，4： | 103 |
| 3 | 金厂沟梁-二道沟金矿田内花岗岩类侵入体锆石的离子探针U-Pb年代学及意义显示文摘金厂沟梁-二道沟金矿田内花岗岩类侵入体SHRIMP锆石U-Ph定年结果表明,该区中生代以来到少经历了三次中酸性岩浆侵入作用,它们分别以西台子二长花岗岩、娄上含辉石石英闪长岩和西对面沟花岗闪长岩及闪长玢岩脉在218±4Ma(印支期)、161±1Ma(燕山早期)和126±1Ma(燕山晚期)的侵位为标志。花岗岩类的地球化学资料表明,这些花岗岩类侵入体形成与造山作用有关,为造山后或陆内拉张作用的产物。二道沟矿区成矿前或成矿期闪长玢岩脉的年龄126±1Ma限定了该区金矿化的最大年龄;结合前人有关年代学资料,认为本区金矿化应发生在126~118Ma。这说明金厂沟梁-二道沟金矿田的金矿床与我国胶东、小秦岭和辽东等地区的金矿床是同时形成的,再次证明燕山晚期是中国最重要而广泛的金成矿期。此外,在这些主要的金矿区内,金矿化时间上均具有与各自区内最晚一次花岗质岩浆作用同时或稍晚的特征,这可能指示金矿床是造山作用或区域构造-岩浆演化最晚期的产物。 | 苗来成 范蔚茗 翟明国 Qiu Y M McNaughton N J Groves D I | 2003 | 岩石学报2003，19，1： | 70 |
| 4 | 哈达门沟金矿床成岩成矿时代的定点定年研究显示文摘哈达门沟大型钾长石 -石英脉型金矿床位于华北地台北缘西段的乌拉山地区。矿区西部的大桦背花岗岩和矿区内的伟晶岩脉与金矿化均具有较为密切的空间关系 ,这导致不少研究者认为哈达门沟金矿床与大桦背岩体或伟晶岩之间也具有时间和成因联系。通过采用先进的高灵敏的高分辨率的离子探针 (SHRIMP)对大桦背岩体、伟晶岩脉和钾长石化蚀变岩进行的锆石 U- Pb定点定年研究表明 :伟晶岩脉形成于 (1836± 5)× 10 6a,属吕梁旋回 ;大桦背岩体形成于 (353± 7)× 10 6a,应为海西旋回早期产物 ;金矿化年龄小于或等于 (132± 2 )× 10 6a,应为燕山晚期。这些年龄结果说明 ,本区金矿化比大桦背岩体晚至少 2 2 0× 10 6a,这排除了金矿化与大桦背岩体和伟晶岩脉之间有任何成因联系的可能性。蚀变岩的年龄还证明 ,虽然乌拉山和胶东地区金矿床的围岩和年龄不同 ,但两地区的金矿化却几乎同时发生。此外 ,大桦背岩体的形成年龄与华北地块和蒙古古陆块碰撞作用发生的时间基本一致 ,因此大桦背岩体的 SHRIMP年龄为这一碰撞作用提供了可靠的年代学证据。 | 苗来成 Yumin Qiu 关康 Neal M cNaughton 裘有守 罗镇宽 David Groves | 2000 | 矿床地质2000，19，2： | 48 |
| 5 | 利用因子分析确定岩溶地下河系统水质的影响因素显示文摘根据云南南洞地下河系统2008年旱季的水化学分析结果,利用因子分析方法探讨地下水水质的影响因素及程度,结果表明:流域地下水成分变动范围较大,具有明显的空间变异性;地下水水质受人类活动、水岩作用过程和土壤等自然因素的共同影响,三个因素能够解释地下水水质形成的79%,其中人类活动是主要影响因素;地下水中的Cl-、NO3-、SO42-、Na+、K+主要受人类活动特别是农业和生活废水等因素的控制,Ca2+主要是水-岩作用的产物,但也受人类活动的影响,pH值、电导率受水岩作用过程和人类活动的影响,Mg2+、HCO3-受土壤CO2含量和水-岩作用过程的共同影响。 | 蒋勇军 吴月霞 Chris Groves 袁道先 Pat Kambesis 李林立 张贵 | 2009 | 水文地质工程地质2009，36，4： | 37 |
| 6 | 内蒙古乌拉山地区大桦背岩体SHRIMP锆石U-Pb年代学研究显示文摘大桦背花岗岩体位于内蒙古乌拉山地区,东距哈达门沟大型钾长石—石英金矿床约5km。前人对该岩体曾做过不少同位素年代学研究,所得结果相差较大,但是多数研究者认为大桦背岩体与区内金矿化具有成因联系。本文采用先进的高灵敏、高分辨率的离子探针(SHRIMP)对大桦背岩体进行了锆石U-Ph定点定年研究。结果表明,大桦背岩体的形成年龄为353±7Ma,应为海西旋回早期产物。此年龄比已得到的乌拉山金矿区成矿年龄大至少70Ma,因而推测大桦背岩体与金矿化之间不存在直接的成因联系。 | 苗来成 Yumin QIU 关康 Neal McNAUGHTON 裘有守 罗镇宽 David GROVES | 2001 | 地质论评2001，47，2： | 34 |
| 7 | 青藏高原北缘中生代伸展构造^(40)Ar/^(39)Ar测年和MDD模拟显示文摘沿着青藏高原北缘的阿尔金山脉东段 ,发育了长度大于 30 0km、EW走向的拉配泉断裂。中美合作阿尔金课题组的地质填图结果表明 ,该断层实际上是一条南倾的正断层 ,局部倾角可以低至 30°以下。沉积学和热年代学研究控制了拉配泉断裂的活动时代 :早—中侏罗统地层可以解释为断裂上盘的伸展盆地沉积 ;下盘岩石中钾长石40 Ar/ 3 9Ar测年和MDD模拟给出 2个阶段的冷却事件 ,早期事件出现在约 2 2 0~ 187Ma之间 ,晚期事件出现在早白垩世晚期 (约 10 0Ma)。早期事件代表了拉配泉断裂正断作用的主要阶段。 | 陈宣华 尹安 George E.Gehrels 王小凤 Eric S.Cowgill Marty Grove T.Mark Harrison 陈正乐 | 2002 | 地球学报2002，23，4： | 30 |
| 8 | SPIRIT 2013声明:定义临床研究方案的标准条目显示文摘临床研究方案是临床研究设计、实行、报告和评价的基础。然而,临床研究方案及现存的临床研究方案指引在内容和质量上差异很大。本文描述了《规范临床研究方案内容》(Standard Protocol Items:Recommendations for Interventional Trials 2013 ),简称SPIRIT2013声明,一个临床研究方案必须报告的条目指引的系统建立和范围。 | An-Wen Chan Jennifer M.Tetzlaff Douglas G.Altman Andreas Laupacis Peter C.GΦtzsche Karmela Krleza-Jeri AsbjΦrn Hróbjartsson Howard Mann Kay Dickersin Jesse A.Berlin Caroline J.Doré Wendy R.Parulekar William S.M.Summerskill Trish Groves Kenneth F.Schulz Harold C.Sox Frank W.Rockhold Drummond Rennie David Moher 钟丽丹 郑颂华 吴泰相 李幼平 商洪才 张伯礼 唐旭东 吕爱平 卞兆祥 | 2013 | 中国循证医学杂志2013，13，12： | 23 |
| 9 | Carbon Fluxes and Sinks:the Consumption of Atmospheric and Soil CO_2 by Carbonate Rock Dissolution显示文摘大陆人区域的碳酸盐岩石露头盖子 9%16% 并且溶解的无机的碳(DIC ) 的主要来源在河边被转移到海洋,后果他们的溶解。当前的评价建议流动在 0.10.6 PgC/a 之间掉落。拿中间的值(0.3 PgC/a ) ,它等于陆上的植被网络碳的 18% 当前的估计下沉, 38% 土壤碳下沉。在中国,从碳酸盐岩石溶解的碳流动被估计是 0.016 PgC/a,它占 21% , 87.5%150% 和 2.3 次森林,灌木和草地分别地捕捞碳水池,以及土壤碳水池流动的 23%40% 。碳酸盐溶解对环境、气候的变化敏感,率密切与降水正在被相关,温度,另外与土壤和植被盖子。水里的 HCO3 被水生植物光合作用影响,被变换成文档和停靠港的 HCO3 部分地结果,它可以由碳酸盐岩石溶解提高碳隐遁的潜力。这碳的可能的周转时间粗略地等于海水周期(2000a ) 的。由碳酸盐岩石溶解的 atmospheric/soil CO2 的举起因此在全球碳周期起一个重要作用,是最重要的水池之一。主要研究需要是更好从碳酸盐矿物质降水与海洋的来源相比评估这个水池的网效果。 | CAO Jianhua YUAN Daoxian Chris GROVES HUANG Fen YANG Hui LU Qian | 2012 | Acta Geologica Sinica(English Edition)2012，86，4： | 20 |
| 10 | Sharing Clinical Trial Data: A Proposal from the International Committee of Medical Journal Editors显示文摘The International Committee of Medical Journal Editors (ICMJE) believes that there is an ethical obligation to responsibly share data generated by interventional clinical trials because participants have put themselves at risk.In a growing consensus,many funders around the world-foundations,government agencies,and industry-now mandate data sharing.Here,we outline ICMJE's proposed requirements to help meet this obligation.We encourage feedback on the proposed requirements.Anyone can provide feedback at www.icmje.org by April 18,2016. | Darren B Taichman Joyce Backus Christopher Baethge Howard Bauchner Peter W de Leeuw Jeffrey M Drazen John Fletcher Frank Frizelle Irish Groves Abraham Haileamlak Astrid James Christine Laine Larry Peiperl Anja Pinborg Peush Sahni Si-Nan Wu | 2016 | Chinese Medical Journal2016，，2： | 20 |
| 11 | Zircon Senstive High Resolution Ion Microprobe (SHRIMP) study of granitoid intrusions in Zhaoye Gold Belt of Shandong Province and its implication显示文摘The zircon Sensitive High Resolution Ion Microprobe (SHRIMP) results show that granitoid intrusions in Zhaoyc Gold Belt were emplaced at two periods of Mesozoic: Linglong and Luanjiahe types of granitic intrusions were emplaced between 160 Ma and 150 Ma (late Jurassic); Guojialing type of granodioritic intrusions, 130 Ma and 126 Ma (early Cretaceous). All the three types contain at least two major generations of inherited zircons with Precambrian ( >650 Ma) and early Mesozoic ages (200-250 Ma), respectively. The former suggests that these plu-tonic rocks are of crustal origin and that Precambrian basement with component of sialic crust up to 3.4 Ga old ( Middle Archean) exists in the region. The presence of abundant inherited zircons with early Mesozoic age indicates that the Precambrian basement was affected by a major tectono-thermal event, that is the collision of the North and South China blocks, at 250 Ma to 200 Ma. SHRIMP results also indicate that the gold mineralization in the region took | 苗来成 罗镇宽 黄佳展 关康 N.J. McNaughton D. I. Groves | 1997 | Science China Earth Sciences1997，40，4： | 15 |
| 12 | Global significance of the carbon cycle in the karst dynamic system:evidence from geological and ecological processes显示文摘On the basis of proposing the existence of a karst carbon cycle and carbon sink at a watershed scale,this paper provides four pieces of evidence for;the integration of geology and ecology during the carbon cycle processes m the karst dynamic system,and estxmated the karst carbon sink effect using the methods of comparative monitoring of paired watersheds and the carbon stable isotope tracer technique.The results of the soil carbon cycle in Maocun,Guilin,showed that the soil carbon cycle in the karst area,the weathering and dissolution of carbonate rocks under the soil,resulted in a lower soil respiration of 25% in the karstoarea than in a non-karst area (sandstone and shale),and the carbon isotope results indicated that 13.46% of the heavy carbon of the hmestone is involved in the soil carbon cycle.The comparative monitoring results m paxred watersheds,suggesting that the HCO3 concentration m a karst spring is 10 times that of a rivulet in a non-karst area,while the concentration of inorganic carbon flux is 23.8 times.With both chemical stoichiometry and carbon stable isotopes,the proportion of carbon in karst springs derived from carbonate rocks was found to be 58.52% and 37.65% respectively.The comparison on carbon exchange and isotopes at the water-gas interface between the granite and carbonate rock basins in the Li River showed that the CO2 emission of the karst water is 10.92 times that of the allogenic water from the non-karst area,while the carbon isotope of HCO3^- in karst water is lighter by 8.62%.However,this does not mean that the karst water body has a larger carbon source effect.On the contrary,it means the karst water body has a greater karst carbon sink effect.When the karst subterranean stream in Zhaidi,Guilin,is exposed at the surface,carbon-rich karst water stimulated the growth of aquatic plants.The values of carbon stable isotopes in the same species of submerged plants gradually becomes heavier and heavier,and the 512 m flow process has a maximum range of 15.46%.The calculation results showed that 12.52% of inorganic carbon is converted into organic carbon.According to the data that has been published,the global karst carbon sink flux was estimated to be 0.53-0.58 PgC/a,equivalent to 31.18%-34.41% of the global forest carbon sink flux.In the meanwhile,the karst carbon sink flux in China was calculated to be 0.051 PgC/a,accounting for 68% of its forest carbon sink flux. | Jian-hua Cao Xia Wu Fen Huang Bill Hu Chris Groves Hui Yang Chun-lai Zhang | 2018 | China Geology2018，1，1： | 9 |
| 13 | 岩溶IGCP国际合作30年与岩溶关键带研究展望显示文摘全球岩溶类型多样,对环境变化敏感,资源与环境问题突出,是地球关键带监测与研究的重点,IGCP661项目的执行为岩溶区关键带类型划分与监测对比研究提供了契机和国际合作平台。近30年岩溶IGCP执行始终强调岩溶系统与人类活动环境的相互作用,其轨迹实际上与地球系统科学到地球关键带理念是一脉相承的。IGCP299提出了岩溶形态组合概念,揭示各种岩溶形态与其形成环境之间的因果关系。岩溶动力系统(IGCP379),岩溶生态系统(IGCP448)概念的提出有助于我们更好地理解岩溶系统的整体功能,及系统内水、生物地球化学过程、人类活动的相互作用,进而形成了一整套岩溶动力学研究方法体系。开辟了岩溶记录与全球变化、碳循环与应对气候变化、石漠化形成演变与生态修复等研究新领域,并取得了丰硕的研究成果,有力地推动了现代岩溶学的发展。 | 章程 蒋忠诚 Chris Groves 袁道先 | 2019 | 中国岩溶2019，38，3： | 9 |
| 14 | 西南岩溶地区地下河水质影响因素的R型因子分析——以桂林寨底地下河为例显示文摘利用R型因子分析法对桂林寨底地下河水化学数据进行分析,识别出影响寨底地下河水质因素的4个主因子:因子1以Ca2+、HCO-3和总硬度为主,表明方解石矿物的溶滤作用对地下水水化学组分的影响;因子2以K++Na+和Cl-为主,反映含水介质易溶盐对水化学组分的重要影响;因子3以SO2-4和NO-3为主,代表了人类活动(农药和化肥的使用、生活污水的污染)对地下水水化学组分的影响作用;因子4以pH和Mg2+为主,反映了弱碱性水环境下白云石矿物的溶滤作用对地下水水化学组分的影响作用。 | 王喆 夏日元 Chris Groves 卢丽 | 2014 | 桂林理工大学学报2014，34，1： | 9 |
| 15 | Proposed case of mesalazine-induced cardiomyopathy in severe ulcerative colitis显示文摘Five-amino salicylic acids are recommended for use in the management of inflammatory bowel disease,cardiac complications are a rare although recognised phenomenon.This report aims to highlight this serious but rare adverse reaction.We report here a case of a young man presenting with cardiogenic shock in the context of recent mesalazine treatment in severe ulcerative colitis. | Kathryn Fleming Andrew Ashcroft Christopher Alexakis Demitrios Tzias Christopher Groves Andrew Poullis | 2015 | World Journal of Gastroenterology2015，21，11： | 9 |
| 16 | 阿尔金山区域热演化历史的初步研究显示文摘通过地质年龄数据的综合分析,本文探讨了阿尔金山地区自元古宙以来的区域热演化历史。其中,本区自古太古代以来具有多期岩浆活动,其主要活动时期为早古生代晚期(490~385 Ma),高峰期年龄为442Ma左右。同时,具有新元古代、早古生代、中生代和新生代4次地壳抬升和冷却事件。其中中生代冷却事件启动时间与阿尔金北缘伸展作用早期活动时间相一致;新生代事件出现在7 Ma左右,与青藏高原隆升具有密切关系。 | 陈宣华 尹安 高荐 George E.GEHRELS 陈正乐 王小凤 Eric S.COWGILL Marty GROVE T.Mark HARRISON | 2002 | 地质论评2002，48，S1： | 8 |
| 17 | 超大型金成矿省的地球动力学背景(摘要)显示文摘 | R. Kerrich R. Goldfarb D. Groves S.Garwin Y. Jia 张静 | 2000 | 中国科学(D辑)2000，30，B12： | 3 |
| 18 | The giant Kalgoorlie Gold Field revisited显示文摘The Neoarchaean Kaigoorlie Gold Field contains the giant Golden Mile and world-class Mt Charlotte deposits,which have been the subject of much research for over 100 years.The Golden Mile deposit is a complex array of ductile to brittle vein and breccia lodes that are predominantly hosted in the highlyfractionated Golden Mile Dolerite sill.The Fimiston lodes comprise an array of narrow lodes that evolved broadly syn- to late-formation of the regional D2 NW-trending foliation.The lodes are characterized by pyrite veinlets and disseminations,quartz veinlets and breccias,and banded quartz-carbonate veins with sericite,carbonate,and pyrite-dominated alteration.Bonanza Green-Leader,or Oroya-style,lodes,with grades in excess of 1000 g/t Au,are similar to the Fimiston-style lodes,but are characterized by abundant visible gold,native tellurium and more abundant telluride minerals within roscoelitebearing alteration zones.The arguably structurally younger Mt Charlotte-style lodes are characterized by a pipe-shaped,coarse-grained quartz,carbonate and scheelite vein-stockwork with distinct verticallyzoned,carbonate-sericite-albite-pyrite ± pyrrhotite dominant alteration assemblages around veins within Unit 8 of the Golden Mile dolerite and porphyry dykes.The network of steep- and gently-dipping extension and shear fracture-fill veins are associated with NE-trending fault sets that cross cut the regional NW-trend.The deposit area is intruded by swarms of porphyry dykes,including syn-volcanic mafic dykes,early and volumetrically most significant c.2.67 Ga feldspar-phyric porphyry dykes,as well as later c.2.66-2.65 Ga calc-alkaline hornblende-phyric dykes associated with younger c.2.65-2.64 Ga lamprophyre dykes.All post-volcanic dykes have similar orientations to the Fimiston lodes.The feldspar dykes are clearly overprinted by all styles of mineralization,although the relationship between hornblende-phyric and lamprophyre dykes and gold mineralization is more ambiguous.Most agree that gold mineralization was post-peak regional metamorphism of host rocks,although its relative structural timing is controversial.Direct timing constraints on gold mineralization indicate that Fimiston- and Mt Charlotte-style mineralization formed within a relative short period of time around 2.64 Ga,and,as such,support a model of progressive deformation of a Theologically heterogeneous rock package late in the structural history.Fluid characteristics,combined with the structural,metamorphic and absolute timing,support description of gold mineralization at the Golden Mile as orogenic and mesozonal,and this allows direct correlation with orogenic gold deposits worldwide,which classically formed during accretion along convergent margins throughout Earth history. | Noreen Mary Vielreicher David Ian Groves Neal Jesse McNaughton | 2016 | Geoscience Frontiers2016，7，3： | 3 |
| 19 | Common variation in the LMNA gene (encoding lamin A/C) and type 2 diabetes - Association analyses in 9,518 subjects显示文摘 | Owen, KR Groves, CJ Hanson, RL Knowler, WC Shuldiner, AR Elbein, SC Mitchell, BD Froguel,P Ng, MCY Chan, JC Jia, WP Deloukas, P Hitman, GA Walker, M Frayling, TM Hattersley, AT Zeggini, E McCarthy, MI | 2007 | 中国生物学文摘2007，21，11： | 2 |
| 20 | Tumour necrosis factor-alpha gene promoter polymorphism and decreased insulin resistence显示文摘 | Day CP Grove J Daly AK | 1998 | Diabetologia1998，41，： | 2 |
您所在的机构暂未开通此部分的功能，请联系管理员