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Application of rock creep experiment in calculating the viscoelastic parameters of earth medium

机译:岩石蠕变实验在计算土介质粘弹性参数中的应用

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Based on the rock creep experiment, the data of aftershock sequence and post-earthquake deformation are used to estimate the viscosity of crust medium near earthquake focus. Firstly 9 samples that belong to 3 kinds of rock are conducted in creep experiment under constant pressure to obtain the creep curves directly. Inversion results show that the standard linear model is the best one to present the earth medium. It exhibits obvious elasticity within a short time, while it exhibits obvious rheology within a long time. The relationship between element module μ_2 and the whole module μ of standard linear model or the module of real earth medium is calculated and analyzed. On the basis of μ_2 = 25 μ, the sequence of aftershock of Gonghe earthquake in Qinghai Province is analyzed and the relationship between accumulated released strain and the time is obtained, which, combined with the creep experiment results, is used to estimate the viscosity of crustal medium in this area. The measured vertical deformation after the same earthquake also is combined with the creep experiment results, then it is used to calculate the relaxation time and viscosity through three different methods respectively, i.e. inversion of Kelvin model, difference method of deformation and viscoelastic dislocation theory. The viscosity of crustal medium in 32 km depth of earthquake focus of Gonghe area deduced from the different data and methods is about 10~(19) Pa·s, which is the same as the research results by other authors at home and abroad.
机译:在岩石蠕变实验的基础上,利用余震序列和震后变形的数据估算了地震震源附近地壳介质的黏度。首先在恒压下进行蠕变实验,对属于3种岩石的9个样品进行直接计算。反演结果表明,标准线性模型是呈现地球介质的最佳模型。它在短时间内表现出明显的弹性,而在长时间内表现出明显的流变性。计算分析了单元模块μ_2与标准线性模型的整个模块μ或真实介质模块之间的关系。在μ_2= 25μ的基础上,对青海省共和地震的余震序列进行了分析,得出了累积释放应变与时间的关系,并结合蠕变实验结果,估算了黏度。该地区的地壳介质。将同一地震后测得的垂直变形也与蠕变试验结果结合起来,然后分别通过三种不同的方法(即开尔文模型反演,变形的差分方法和粘弹性位错理论)来计算松弛时间和黏度。根据不同的资料和方法推算,共和地区地震震源深32 km处的地壳黏度约为10〜(19)Pa·s,与国内外其他学者的研究结果相同。

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