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13篇 您的检索式:作者名="KIRBY Eric"
    题名 作者 年代 出处 被引量
1Spatial differences in rock uplift rates inferred from channel steepness indices along the northern flank of the Qilian Mountain,northeast Tibetan Plateau显示文摘The rate and distribution of deformation along the Qilian Mountain,on the northeastern Tibetan Plateau,is needed to understand the evolution of high topography associated with the plateau.Recently,a number of empirical studies have provided support for the contention,common to most models of fluvial incision,that rock uplift rate exerts a first-order control on the gradient of longitudinal river profiles.Along the northern Qilian Mountain,this method is used to extract information about the spatial patterns of differential rock uplift.Analysis of the longitudinal profiles of bedrock channels reveals systematic differences in the channel steepness index along the trend of the frontal ranges.Local comparisons of channel steepness reveal that lithology and precipitation have limited influence on channel steepness.Similarly,there is little evidence suggesting that channel steepness is influenced by differences in the sediment loads.We argue that the distribution of channel steepness in the Qilian Mountain is mostly the result of differential rates of rock uplift.Thus,channel steepness indices reveal a lower rock uplift rate in the eastern portion of the Qilian Mountain and a higher rate in the middle and west.The highest rates appear to occur in the middle-west portions of the range,just to the west of the Yumu Shan.HU XlaoFei PAN BaoTian KIRBY Eric LI QingYang GENG HaoPeng CHEN JiFeng 2010Chinese Science Bulletin2010,55,27:35
2Strategic Groups and outcomes in the US hospice care industry显示文摘Eric G Kirby 2012Journal of Health Organization and Manage- ment2012,26,5:1
3Free-living physical activity in COPD: Assessment with accelerometer and activity checklist显示文摘Moy Marilyn L Matthess Kirby Stolzmann Kelly Reilly John Garshick Eric 2009Journal of Rehabilitation Research and Development2009,,2:1
4Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin显示文摘Tom Parsons Chen Ji Eric Kirby 2008Nature2008,454,:1
5Stress changes from the2008 Wenchuan earthquake and increased hazard in the Sichuan basin显示文摘Tom Parsons Chen Ji Eric Kirby 2008Nature2008,454,50:1
6Stress changes from the 2008 Wenchuan Earthquake and iincreased hazard in the Sichuan Basin 显示文摘Parsons T C hen J Eric Kirby 2008Nature2008,454,7203:1
7Late Cenozoic evolution of the eastern margin of the Tibetan Plateau 显示文摘Eric Kirby Peter W Reiners 2002Tectonics2002,21,1:1
8A re- vised chronology for Tertiary sedimentation in the Sikouzi basin: Implications for the tectonic evolution of the northeastern comer of the Tibetan Plateau显示文摘Wang Weitao Zhang Peizhen Eric Kirby 2011Tectono- physics2011,505,1234:1
9Along-strike topographic variation of the Longmen Shan and its significance for landscape evolution along the eastern Tibetan Plateau 显示文摘Hui-ping Zhang Pei-zhen Zhang Eric Kirby Jin-hui Yin Chun-ru Liu Gui-hua Yu 2010Journal of Asian Earth Sci- ences2010,40,4:1
10Costs for electric-power ancillary services显示文摘ERIC HIRST BRENDAN KIRBY 1996The Electricity Journal1996,9,10:1
11Key Transmission Planning Issues 显示文摘Eric Hirst Brendam Kirby 2001The Electricity Journal2001,14,8:1
122008年汶川地震造成的应力变化与四川盆地危险性的增加显示文摘2008年5月12日,汶川特大地震袭击了西藏高原东部边界地区,对中国四川盆地西部的主要城市产生影响,造成数千人死亡。如此之大的地震过后,地壳中应力的重新分布通常会导致随后一系列破坏性地震的发生。5月12日的主震破裂造成龙门山和四川盆地之间的边界高达9m的滑移,呈现了复杂的走滑和逆冲运动。四川盆地及周边地区也被其他走滑逆冲活动断层穿越。在这里,我们提出了使用这些断层模型来计算5月12日地震引起的同震应力变化,并显示出许多显著的应力增加。及时地绘出应力变化图可以帮助找出产生余震可能性相对较高的断层段。Tom Parsons Chen J Eric Kirby 王璞(翻译) 黄禄渊(校对) 2018地壳构造与地壳应力2018,0,1:0
13沿龙门山构造带走向上地形发育差异特征及其对青藏高原东缘地貌演化的启示显示文摘2008年5月12日,沿青藏高原东缘龙门山构造带内部的中央及前山断裂发生了慨8.0级强烈地震,两条同震地表破裂带分别达240km和72km。野外调查及震源破裂过程反演得到同震破裂样式表现为沿走向上的差异特征,其中同震破裂的南段(映秀-北川)以逆冲运动为主,走滑运动为辅,然而北段(北川以北)则表现为走滑运动为主。这一同震破裂分段特征促使我们进一步审视该过程是否对龙门山构造带的地形演化起到了控制作用。张会平 张培震 Eric Kirby 尹金辉 刘春茹 于桂华 2012国际地震动态2012,,6:0
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