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您的检索式：作者名="K.M.Larson"
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| 1 | 中国大陆现今地壳运动和构造变形显示文摘全球定位系统(GPS)揭示的中国大陆现今运动场清晰地表现出了以活动地块 为单元的分块运动特征,不同的活动地块具有不同的运动和变形方式.GPS观测到的阿 尔金断裂的左旋走滑速率仅(5.l± 2.5)mm/a,龙门山断裂的挤压缩短速率为(6.7± 3.0) mm/a,华南地块相对于欧亚大陆向东的运动速率是 11~14mm/a,这些结果均不支持青 藏高原北部沿主要走滑断裂向东大规模挤出的假说.中国大陆以活动地块为单元的现 今构造变形可能与大陆岩石圈的结构和性质有关,上地壳以脆性变形为主,下地壳和 上地幔以粘塑性的流变为特征,从底部驱动着上覆脆性地块的整体运动. | 王琪 张培震 牛之俊 J.T.Freymueller 赖锡安 李延兴 朱文耀 刘经南 R.Bilham K.M.Larson | 2001 | 中国科学(D辑)2001，31，7： | 189 |
| 2 | Present-day crustal movement and tectonic deformation in China continent显示文摘Velocity field of China continent constrained by Global Positioning System (GPS) reveals both continuous and block-like styles of deformation. Continuous deformation commonly characterizes actively deforming mountain ranges such as the Tianshan Mountain, Qilian Mountain, and Tibet. The block-like movement often represents deformation in the tectonically stable regions such as Ordos, South China and Tarim blocks. GPS measurements indicate 5.1±2.5 mm/a left-lateral strike-slip rate along the Altun fault. Eastward convergence along the Longmenshan fault is less than 6.7±3.0 mm/a. South China moves 11-14 mm/a eastward compared with the stable Eurasia. These low slip rates do not imply rapid eastward extrusion of China continent predicted by the model of 'continental extrusion'. It appears that 'crustal thickening' model more properly describes both continuous and block-like styles of deformation in China continent. | 王琪 张培震 牛之俊 赖锡安 J.T.Frevmueller 朱文耀 刘经南 李延新 R.Bilham K.M.Larson | 2002 | Science China Earth Sciences2002，45，10： | 10 |
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