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- W2364401059 abstract "Obvious differences exist in the complexity of Pm waves obtained by deep seismic sounding (DSS) in different tectonic units. These differences are closely related to deep structural features. In this paper, a method is proposed for computing the complexity of seismic waves on the basis of its transient features and duration. For an ancient stable block, the Moho complexity coefficient is small, which reflects the feature of first order discontinuous interface. In contrast, for a strongly active block, the Moho complexity coefficient is large, which reflects the feature of crust-mantle transitional zone. Data processing was carried out with respect to a DSS profile which passes through the northeastern edge of Qinghai-Xizang Plateau. The result was interpreted dynamically." @default.
- W2364401059 created "2016-06-24" @default.
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- W2364401059 date "2005-01-01" @default.
- W2364401059 modified "2023-09-25" @default.
- W2364401059 title "COMPLEXITY FEATURE OF CRUST-MANTLE TRANSITIONAL ZONE AND ITS DYNAMIC IMPLICATIONS" @default.
- W2364401059 hasPublicationYear "2005" @default.
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