摘要 : Rocks are heterogeneous materials. Deformation structures and fabrics in the ductile lithosphere can result from the history of the three dimensional flow field, or the progressive deformation of some rheologically distinct elemen... 展开
作者 | Jiang~ DZ |
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作者单位 | |
期刊名称 | 《Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth》 |
总页数 | 15 |
语种/中图分类号 | 英语 / P54 |
关键词 | Flow on a surface Vorticity decomposition Sectional vorticity number Sectional dilatancy number Kinematic analysis Finite deformation |
馆藏号 | N2008EPST0001329 |