青藏高原均衡重力异常的地震构造动力学研究
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摘要
根据Airy-Hesikannen均衡假说,以CRUST2.0模型提供的密度和Moho面深度作为计算参数,计算得到青藏高原的均衡重力异常,并结合地震资料从均衡的角度对青藏高原的地震构造动力学进行了解释。研究表明,强震往往发生在均衡重力异常梯度带等值线的斜坡带、陡变带以及拐弯区上,说明地壳构造与地震的发生有一定的关系。
On the basis of the Airy-Hesikannen equilibrium hypothesis,the isostatic gravity anomalies of Qinghai-Tibet plateau are calculated taking the density and the depth of upper lithosphere from the CRUST2.0 model as parameters,and then the seismo-tectonic dynamics is studied by use of the seismic data from the point of equilibrium.It shows that strong earthquakes occur often in the inflexion of gradient belt of isostatic gravity anomalies,and generally,the occurrence of earthquake is correlated to crust tectonics.
引文
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