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26篇 您的检索式:作者名="Nigel Harris"
    题名 作者 年代 出处 被引量
1西秦岭花岗岩类地球化学和Pb-Sr-Nd同位素组成对基底性质及其构造属性的限制显示文摘对西秦岭印支期5个花岗岩类岩体进行了岩石主量元素、微量元素和Pb-Sr-Nd同位素地球化学的研究, 据此限定西秦岭的地壳基底性质及其构造属性. 结果表明, 西秦岭花岗岩类总体化学成分偏基性, 岩石主要属于准铝质的高钾-钾玄质系列, A/CNK=0.90~1.05 (绝大多数样品<1.0), K2O/Na2O=1.04~1.86. 它们具有相似的微量元素(包括稀土元素)组成模式, (La/Yb)N= 7.49~ 28.79, Eu*/Eu=0.39~0.76. 在Sr-Nd同位素组成上, 西秦岭花岗岩显示一定程度的不均一性, ISr= 0.70682~0.70845, εNd(t)=-4.85~-9.17, TDM=1.26~1.66 Ga. 西秦岭花岗岩类以高放射成因铅同位素组成为特征, 其初始铅同位素比值为: 206Pb/204Pb=17.996~18.468, 207Pb/204Pb=15.565~15.677, 208Pb/204Pb=38.082~38.587. 根据西秦岭花岗岩类的化学和Sr-Nd同位素组成, 揭示了它们的岩浆源区均来自于地壳中高K(Rb)玄武质岩石的部分熔融, 源区物质形成时代可能在900~1400 Ma之间, 由此反映在西秦岭沉积盖层之下含有大量的中、新元古代的高K (Rb)玄武质岩层. 西秦岭印支期花岗岩类与东秦岭印支期花岗岩类的Pb-Sr-Nd同位素组成对比, 指示西秦岭和东秦岭地壳具有不同的基底组成, 两者的分界线大至位于近南北向的宝成铁路线. 西秦岭花岗岩类Pb-Nd同位素组成特征表明西秦岭地壳基底具有扬子块体的构造属性.张宏飞 靳兰兰 张利 Nigel Harris 周炼 胡圣虹 张本仁 2005中国科学(D辑)2005,35,10:130
2北喜马拉雅淡色花岗岩地球化学:区域对比、岩石成因及其构造意义显示文摘北喜马拉雅出露一系列片麻岩穹窿,这些穹窿被形成于27.5~10Ma的淡色花岗岩侵入.淡色花岗岩的岩石类型为二云母花岗岩,它们的主量元素组成为SiO2=70.97%~74.54%、K2O+Na2O=6.27%~8.09%、K2O/Na2O=0.91~1.36及A/CNK=1.10~1.33.然而,它们在微量元素组成上呈现出较大的变化:Rb=(41~322)×10-6、Sr=(26~139)×10-6、Ba=(135~594)×10-6、(La/Yb)N=0.97~17.31、Eu/Eu=0.29~0.72.北喜马拉雅淡色花岗岩的主量元素和微量元素组成特征类似于高喜马拉雅中新世的二云母花岗岩,而在Ti、Mg、Ca、Ba含量和Rb/Sr比值上明显不同于高喜马拉雅中新世的电气石-白云母花岗岩.北喜马拉雅淡色花岗岩(87Sr/86Sr)t=0.7344~0.8503(t=10Ma),εNd(10Ma)=-12.5~-19.3,与高喜马拉雅淡色花岗岩无明显差异.在岩石成因上,北喜马拉雅和高喜马拉雅中新世淡色花岗岩均起因于构造减压作用,由此导致白云母发生脱水反应诱发高喜马拉雅结晶岩系的深熔.但北喜马拉雅淡色花岗岩形成的地质背景明显不同于高喜马拉雅淡色花岗岩,前者具有较长的时间跨度,开始形成于喜马拉雅渐新世的地壳增厚期,之后形成于中新世穹窿片麻岩的折返时期,而高喜马拉雅淡色花岗岩与中新世高喜马拉雅结晶岩系的构造挤出作用有关.因此。张宏飞 Nigel Harris Randall Parrish 张利 赵志丹 李德威 2005地球科学(中国地质大学学报)2005,30,3:65
3Geochemical and Pb-Sr-Nd isotopic compositions of granitoids from western Qinling belt: Constraints on basement nature and tectonic affinity显示文摘Geochemical and Pb-Sr-Nd isotopic compositions of five Indosinian granitoid intrusions from the western Qinling belt provide insights into basement nature and tectonic affinity. The results show that the western Qinling granitoids incline towards basic in their bulk chemical composition. The granitoids belong to high-K to shoshonitic series with K2O/Na2O=1.04-1.86 and are dominantly metaluminous with A/CNK=0.90-1.05 (most samples have A/CNK of <1.0). They have similar trace elemental compo- sitional patterns. In Sr-Nd isotopic compositions, they display some extent heterogeneity with Isr=0.70682-0.70845, εNd(t)=?4.85 to ?9.17 and TDM=1.26-1.66 Ga. They are characterized by high ra- diogenic Pb isotopic compositions. Their initial Pb isotopic ratios are 206Pb/204Pb=17.996-18.468, 207Pb/204Pb=15.565-15.677 and 208Pb/204Pb=38.082-38.587. Geochemical and Sr-Nd isotopic composi- tions reveal that magma for the granitoids was derived from partial melting of high-K (Rb) basaltic rocks, which might be formed in 900-1400 Ma. It is suggested that a large amount of the Proterozoic high-K (Rb) basaltic rocks, which underlie the Phanerozoic sedimentary cover, constitute the crustal basement of the western Qinling belt. Pb-Sr-Nd isotopic compositional comparison between the east- ern Qinling and the western Qinling Indosinian granitoids indicates that the crustal basement of the western Qinling is distinct from that of the eastern Qinling. The Baoji-Chengdu railway close to south-north orientation can be taken as an approximate boundary between both basements. The Pb-Nd isotopic compositional characteristics of the western Qinling granitoids suggest that the basement of the western Qinling belt has an affinity with the Yangtze block.Nigel HARRIS 2007Science China Earth Sciences2007,50,2:33
4A history of high-power laser research and development in the United Kingdom显示文摘The first demonstration of laser action in ruby was made in 1960 by T.H.Maiman of Hughes Research Laboratories,USA.Many laboratories worldwide began the search for lasers using different materials,operating at different wavelengths.In the UK,academia,industry and the central laboratories took up the challenge from the earliest days to develop these systems for a broad range of applications.This historical review looks at the contribution the UK has made to the advancement of the technology,the development of systems and components and their exploitation over the last 60 years.Colin N.Danson Malcolm White John R.M.Barr Thomas Bett Peter Blyth David Bowley Ceri Brenner Robert J.Collins Neal Croxford A.E.Bucker Dangor Laurence Devereux Peter E.Dyer Anthony Dymoke-Bradshaw Christopher B.Edwards Paul Ewart Allister I.Ferguson John M.Girkin Denis R.Hall David C.Hanna Wayne Harris David I.Hillier Christopher J.Hooker Simon M.Hooker Nicholas Hopps Janet Hull David Hunt Dino A.Jaroszynski Mark Kempenaars Helmut Kessler Sir Peter L.Knight Steve Knight Adrian Knowles Ciaran L.S.Lewis Ken S.Lipton Abby Littlechild John Littlechild Peter Maggs Graeme P.A.Malcolm OBE Stuart P.D.Mangles William Martin Paul McKenna Richard O.Moore Clive Morrison Zulfikar Najmudin David Neely Geoff H.C.New Michael J.Norman Ted Paine Anthony W.Parker Rory R.Penman Geoff J.Pert Chris Pietraszewski Andrew Randewich Nadeem H.Rizvi Nigel Seddon MBE Zheng-Ming Sheng David Slater Roland A.Smith Christopher Spindloe Roy Taylor Gary Thomas John W.G.Tisch Justin S.Wark Colin Webb S.Mark Wiggins Dave Willford Trevor Winstone 2021High Power Laser Science and Engineering2021,9,2:5
5Decompression and anatexis of Himalayan metapelites显示文摘Nigel Harris John Massey 1994Tectonics1994,13,6:1
6Agent-based semantic Web services显示文摘Nicholas Gibbins Stephen Harris Nigel Shadbolt 2004Journal of Web Semantics:Science Services and Agents on the World Wide Web2004,1,1:1
7Channel flow and the Himalayan Tibetan orogenoA critical review显示文摘Nigel Harris 2007Geological Society2007,164,3:1
8ln a Global Economy Structural Adjustment and the Role of Cities显示文摘Harris Nigel 1995Cities1995,,12:1
9Mapping granite and gneiss in domes along the North Himalayan antiform with ASTER SWIR band ratios显示文摘Doyle R Watts Nigel B Harris W 0,,:1
10Bombay in a Global Economy-Structural Adjustment and the Role of Cities显示文摘Harris Nigel 1995Cities1995,12,3:1
11U–Pb zircon ages, geochemical and isotopic compositions of granitoids in Songpan-Garze fold belt, eastern Tibetan Plateau: constraints on petrogenesis and tectonic evolution of the basement显示文摘Hong-Fei Zhang Li Zhang Nigel Harris Lan-Lan Jin Honglin Yuan 2006Contributions to Mineralogy and Petrology2006,,1:1
12U–Pb zircon ages, geochemical and isotopic compositions of granitoids in Songpan-Garze fold belt, eastern Tibetan Plateau: constraints on petrogenesis and tectonic evolution of the basement显示文摘Hong-Fei Zhang Li Zhang Nigel Harris Lan-Lan Jin Honglin Yuan 2006Contributions to Mineralogy and Petrology2006,,1:1
13Bombay In A Global Economy--Structural Adjustment And The Role Of Cities 显示文摘Harris Nigel 1995Cities1995,12,3:1
14U-Pb zircon SHRIMP ages, geochemical and Sr-Nd-Pb isotopic compositions of intrusive rocks from the Longshan-Tianshui area in the southeast corner of the Qilian orogenic belt,China: Constraints on petrogenesis and tectonicaitinity显示文摘Zhang H F Zhang B R Nigel Harris 2006Journal of Asian Earth Sciences2006,27,:1
15The nematicidal effects of the bacteria Pseudomonas oryzihabitans and Xenorhabdus nematophilus on the root-knot nematode Meloidogyne javanica显示文摘Harry Y. Samaliev Fotini I. Andreoglou Sami A. Elawad Nigel G.M. Hague Simon R. Gowen 2000Nematology2000,,5:1
16Trace ele- ment discrimination diagram for the tectonic interpretation of gra-nitic rocks显示文摘Pearce Julian A Harris Nigel B W Tindle Andrew G 1984Journal of Petrology1984,25,4:1
17Geochemicalcharacteristics of collision- zone magmatism显示文摘Harris Nigel Bw Pearce Julian A Tindle Andrew G 1986Geological Society London Special Publications1986,19,1:1
18The marginal profitability of train services in London显示文摘Nigel G Harris 1996Transport Policy1996,13,12:1
19Urbanization, economic development and Policy in developing countries 显示文摘Nigel Harris 1990Habitat International1990,14,4:1
20U–Pb zircon ages, geochemical and isotopic compositions of granitoids in Songpan-Garze fold belt, eastern Tibetan Plateau: constraints on petrogenesis and tectonic evolution of the basement显示文摘Hong-Fei Zhang Li Zhang Nigel Harris Lan-Lan Jin Honglin Yuan 2006Contributions to Mineralogy and Petrology2006,,1:1
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