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| 1 | 青藏高原东部及周边现时地壳运动显示文摘通过1991—2001年期间在青藏高原东部及周边地区的GPS测量,获得该地区不同参考框架下的地壳运动速度场,其测量的速度精度高于2mm/yr。印度板块与华北地块之间的地壳形变分为喜马拉雅及高原南部、高原中部(拉萨—格尔木)和高原北部(格尔木—金塔)三部分,它们分别吸收了印度板块与欧亚板块汇聚速率的43%、24%和32%。在欧亚框架下和相对于成都,印度板块和华南地块之间存在着以东喜马拉雅构造结为轴心的顺时针巨型涡旋构造———滇藏涡旋构造,运动速度分别为26~6mm/yr和24~7mm/yr,总体上从北东方向转变为南东和南西方向,有别于青藏高原中部的北东方向。滇藏涡旋和东喜马拉雅构造结的形成与南迦巴瓦 阿萨姆'犄角'的楔入作用有关。 | 刘宇平 陈智梁 唐文清 赵济湘 张选阳 张清志 Robert W. King Burrcel C. Burchfiel Leigh H. Royden | 2003 | 沉积与特提斯地质2003，23，4： | 14 |
| 2 | 青藏高原的地质学演化显示文摘 | L. H. Royden B.C. Burchfiel R.D. van der Hilst 李安(译) 石峰(译) 王椿镛(校) | 2009 | 世界地震译丛2009，40，3： | 2 |
| 3 | Surface deformation and lower crustal flow in eastern Tibet显示文摘 | ROYDEN L H BURCHFIEL B C KING R W et al | 1997 | Science1997，276，： | 1 |
| 4 | Nature Geoscience:双俯冲系统使印度板块向欧亚大陆的俯冲速度加快显示文摘2015年5月4日,NatureGeoscience杂志发表了题为《双俯冲系统使印度板块向欧亚大陆的俯冲速度加快》(Anomalously fast convergence of India and Eurasiacaused bydouble subduction)的文章,指出地幔中的双重俯冲作用导致一个构造板块向另一个板块之下俯冲,拖动着印度向北迁移,板块下沉的同时拉动与其连接的大陆。地质学家推断,两个板块的下沉提供了双倍的拖拽力,从而导致印度的漂移速度加倍。 | 赵纪东 王艳茹 Jagoutz O Royden L Holt A F | 2015 | 国际地震动态2015，36，6： | 1 |
| 5 | Rifting process and thermal evaluation of the continental margin of eastern Canada determined from subsi-dence curves显示文摘 | Royden L Keen C E | 1980 | Earth and Planetary Science Letter1980，51，： | 1 |
| 6 | Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patterns 显示文摘 | Clark M K Schoenbohm L M Royden L H | 2004 | Tectonics2004，23，： | 1 |
| 7 | Topographic ooze:Building the eastern margin of Tibet by lower crustal flow显示文摘 | CLARK M K ROYDEN L H | 2000 | Geology2000，28，： | 1 |
| 8 | Motion of the Pacific plate relation to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia显示文摘 | Northrup C J Royden L H Burehfiel B C | 1995 | Geology1995，23，： | 1 |
| 9 | Motion of the Pacific plate relation to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia显示文摘 | Northrup C J Royden L H Burchfiel B C | | Geology0，23，： | 1 |
| 10 | Surface uplift,tectonics and erosion of Eastern Tibet from large-scale drainagepatterns显示文摘 | Clark M K Schoenbohm L M Royden L H | 2004 | Tectonics2004，23，： | 1 |
| 11 | Surface deformation and lower crustal flow in Tibet 显示文摘 | Royden L H Burhfiel B C King R W | 1997 | Science1997，276，： | 1 |
| 12 | Motion of the Pacific plate relative to Eurasia and its optional relation to Cenozoic extension along the eastern margin of Eurasia显示文摘 | NORTHRUP C J ROYDEN L H BURCHFIEL B C | 1995 | Geology1995，23，： | 1 |
| 13 | Transesterification kinetics of soybean oil 显示文摘 | Bernard F Royden O BUtterfied | 1986 | American Oil Chemists:Society1986，63，10： | 1 |
| 14 | Transesterification kinetics of soybean oil 1显示文摘 | Bernard Freedman Royden O. Butterfield Everett H. Pryde | 1986 | Journal of the American Oil Chemists’ Society1986，，10： | 1 |
| 15 | Surface deforrna tion and lower crustal flow in Eastern Tibet显示文摘 | Royden L H Burchfiel B C King R W | 1997 | Science1997，276，： | 1 |
| 16 | Surface deformation and lower crustal flow in Eastern Tibet 显示文摘 | Royden L H Burchriel B C King R W | 1997 | Science1997，276，： | 1 |
| 17 | Late Cenozoic uplift of southeastern Tibet显示文摘 | Clark M K House M A Royden L H Whipple K X Burchfiel B C Zhang X Tang W | 2005 | Geology2005，33，6： | 1 |
| 18 | Late Cenozoic uplift of southeastern Tibet显示文摘 | CLARK M K HOUSE M A ROYDEN L H et al | 2005 | Geology2005，33，： | 1 |
| 19 | Large-scale crustal deformation of the Tibet Plateau显示文摘 | Shen F Royden L H Burchfiel B C | 2001 | Journal of Geophysical Research2001，106，4： | 1 |
| 20 | Surface deformation and lower crustal flow in eastern Tibet显示文摘 | Royden L H Burchfiel B C King R W | | 0，，5313： | 1 |
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