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175篇 您的检索式:作者名="G Hilton"
    题名 作者 年代 出处 被引量
1龙门山北段平通河流域地貌演化过程显示文摘龙门山位于青藏高原东缘,是青藏高原周缘山脉中陡度变化最大的山脉,也是全球气候和构造活动最为强烈的地区之一,因此成为研究构造、气候如何影响山脉地貌演化过程这一科学问题的良好素材。在位于龙门山北段的平通河流域,汶川地震导致该区强烈的隆升、剥蚀作用,对研究该区地貌演化过程具有重要的启示意义。通过对平通河流域基于DEM数据的地形坡度、水系分布、河流发育程度等的分析,并综合研究区构造特征和岩性特征,获得该流域不同区域的地貌演化方向,其中两个区域的地貌演化最为剧烈:1.平通河流域位于北川-映秀断裂和彭灌断裂之间的地区,未来将发生较快的隆升,地貌向高、陡的方向演化,河流下切作用使河谷两岸形成更加陡峭的地形;2.在北川-映秀断裂上盘附近地区,在构造和气候作用下侵蚀、搬运作用强烈,山体将被快速剥蚀削低,但在河谷两岸也会形成更加陡峭的地形。颜照坤 李勇 黄润秋 李奋生 闫亮 赵国华 张自力 张威 Densmore A L Hilton R G 2012山地学报2012,30,2:5
2汶川地震对龙门山地区平通河河流系统沉积物输移的影响显示文摘通过对龙门山地区2008年9月和2010年8月发生的大规模的滑坡和泥石流地质灾害的实地考察,并在详细分析龙门山北段平通河地震前后输沙率变化情况的基础上,对龙门山地区2008年汶川地震驱动的地质灾害空间分布情况、龙门山地区地形地貌特征和龙门山地区降水空间分布情况作对比分析,获得以下认识:①汶川地震对该区地质灾害的影响将是持续的,震后地质灾害形成的松散物源将以河流为载体,被输送到下游,并对下游水利建设、防洪防涝等产生较大影响;②构造因素(汶川地震)和地形地貌因素为地质灾害发生的根本原因,气候(降水量和降水强度)则为直接诱发因素。颜照坤 李勇 黄润秋 林伟 李奋生 DENSMORE Alexander L HILTON Robert G 2011自然杂志2011,33,6:3
3Extreme 3He/4He ratios in northwest Iceland:constratining the common component in mantle plumes 显示文摘Hilton D R Gronvold K Macpherson C G 1999Earth Planet Sci Lett1999,173,:2
4Novel 1xN and NxN Integrated Optical Switches Using Self-lmaging Multimode GaAs/Al-GaAs Waveguides显示文摘Jenkins R M Heaton J M Wright D R Parker J T Birbeck J C H Smith G W Hilton K P 1994Appl Phys Lett 71994,64,:1
5The emerging role of avian cytokines as immunotherapeutics and vaccine adjuvants 显示文摘Hilton L S Bean A G Lowenthal J W 2002Veterinary Immunology and Immunopathology2002,85,34:1
6Factoring the environmental Kuznets Curve:evidence from automotive emissions显示文摘HILTON F G H A LEVINSON 1998Joumal of Environmental Economics and Management1998,35,:1
7Relevance of enantiomeric separations in environmental science显示文摘Amstrong D W Reid G L Ill Hilton M L 1993Environ Pollut1993,79,:1
8The emerging role of avian cytokines as immunother-apeutics and vaccine adjuvants显示文摘Hilton L S Bean A G Lowenthal J W 2002Vet Immunol Immunopathol2002,85,34:1
9Helium4 characteristics of groundwaters from central Australia: Comparative chronology with chlorine-36 and carbon-ld dating techniques显示文摘KULONGOSKI J T HILTON D R CRESSWELL R G 2008Journal of Hydrology2008,348,:1
10Diagnosing foot infections in diabetes显示文摘Williams D T Hilton J R Harding K G 2004Clin Infect Dis2004,39,2:1
11Transmission and accumulation of CTL escape variants drive negative associations between HIV polymorphisms and HLA显示文摘Leslie A Kavanagh D Honeyborne I Pfafferott K Edwards C Pillay T Hilton L Thobakgale C Ramduth D Draenert R Le Gall S Luzzi G Edwards A Brander C Sewell A K Moore S Mullins J Moore C Mallal S Bhardwaj N Yusim K Phillips R Klenerman P Korber B Kiepiela P Walker B Goulder P 2005J Exp Med2005,201,6:1
12Interleukin-2 directly induces activation and proliferation of chicken T cells in vivo显示文摘Hilton L S Bean A G Kimpton W G 2002J Interferon Cytokine Res2002,22,7:1
13The isotopic composition of particulate organic carbon in mountain rivers of Taiwan 显示文摘Hilton R G Galy A Novius N 2010Geohimica et Cosmochimiea Acta2010,74,:1
14Chceklists and muhidisciplinary team performance during simulated ob- stetric hemorrhage显示文摘Hilton G Danicls K Goldhaber- Fiebcrt SN Int J Obstet Anesth0,21,:1
15Factoring the environmental Kuznets Curve: Evidence from automotive emissions 显示文摘Hilton F G H Levinson A 1998Journal of Environmental Economics and Management1998,35,:1
16Reducing the dimensionality of data with neural networks 显示文摘Hilton G G Salakhutdinov R R 2006Science2006,313,:1
17Factoring the environmental kuznets curve: evidence from automobile lead emission显示文摘HILTON F G H LEVINSON A 1998Journal of Environmental Economics and Management1998,35,2:1
18Finite-difference time-domain analysis of a printed dipole antenna显示文摘HILTON G S RAILTON C J BALL G J 1995Antennas and Propagation1995,407,:1
19Factoring the Environmental Kuznets Curve: Evidence from Automotive Lead Emissions显示文摘Hilton F G Levinson A 1998Journal of Environmental Economics and Management1998,35,:1
20Carbon nanotube terahertz polarizer 显示文摘ACS Applied PEN L PINT C L BOOSHEHRI L G RICE W I3 WANG X HILTON D J TAKEYA K KAWAYAMA I TONOUCHI M HAUGE R H KONO J 2009Nano Letters2009,9,7:1
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