Fractal and electromagnetic properties of shear zones and the state-of-stress problem

1.剪切带的分形性和电磁特性分析：利用科学研究助学金(10740235)购买的介电常数测试仪，研究了断层岩介电常数的分形性和电磁特性(即介电常数、IR、CL和TL)。根据青年科学家和科学研究助学金(07854024、08740389、10740235和12640436)的结果，本研究提出了断层各参数与断层岩石的分维和电磁性质之间的一些关系。讨论了它们的性质与剪切带变形的关系。2.剪切带的地质压力计和应变计：基于剪切带的微分几何与物理场(物理相互作用场)的关系，提出了剪切带的分维特性与电磁特性之间的关系。提出了天然断层岩石的非线性磨损模型和断层岩石的地质压力计，研究了地壳岩石的非线性瞬变力学行为和时间-温度叠加原理。3.岩石圈的强度和应变以及真实剪切带模型：基于断层岩石的分维和电磁特性，研究了剪切(断层)带的各种物理条件。利用断层岩石压力计和应变仪对岩石圈的强度和应变进行了估算，解决了岩石圈的应力状态问题，为剪切(断层)带提供了一个真实的模型。此外，基于断裂岩的分维和电磁性质，研究了应力状态下剪切(断裂)带的电磁结构(电位)及其来源。其中一些成果已经发表，其他成果现已提交国际期刊出版。

1.Analysis of the fractal and electromagnetic properties of shear zones : By using the apparatus of dielectric permittivity which were bought by Grant-in-Aid for Scientific Research (10740235), I studied the fractal and electromagnetic properties (i.e., dielectric permittivities, IR,CL and TL) of fault rocks. From the results from the Grant-in-Aids for Encouragement of Young Scientist and Scientific Research (07854024,08740389,10740235 and 12640436), this study proposed some relationships among each parameter on faults and the fractal and electromagnetic properties of fault rocks. Moreover, some relations between their properties and deformation of shear zones were discussed.2.Geological piezometer and strain-meter of shear zone : Based on the relation between the differential geometry and physical field (physical interaction filed), the relationships between the fractal and electromagnetic properties of shear zones were proposed. Moreover, a nonlinear wear model of natural fault rocks and a geological piezometer of fault rocks were proposed, and a nonlinear transient mechanical behavior and time-temperature superposition principle of crustal rocks were investigated.3.Strength and strain of lithosphere and a real shear zone model : Based on the fractal and electromagnetic properties of fault rocks, the various physical conditions of shear (fault) zones were investigated. Using the piezometer and strain-meter of fault rocks, the strength and strain of lithosphere were estimated, and this research cleared the state-of-stress problem in order to propose a real model for shear (fault) zones. Moreover, based on the fractal and electromagnetic properties of fault rocks, the electromagnetic structures (potentials) and their sources in shear (fault) zones induced in the state-of-stress were investigated. Some of these results have been published and others are now submitted for the publication of international journals.