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Moreover, there are 3∼6 distinct interfaces in the shallow velocity structure (0∼1000 m).
Also, the shallow velocity structure (0∼ 1000 m) can be roughly divided into 3 6 layers.
There are 3∼6 distinct interfaces in the shallow velocity structure (0∼1000 m).
The shallow velocity structure of the Chianan plain was investigated using the microtremor array analysis (Kuo et al. 2016a).
Di Giulio et al. (2006) deployed five small-aperture array measurements of microtremors to study wave-field properties and shallow velocity structures in the Colfiorito plain, Italy.
Compared to the direct borehole method, non-intrusive surface methods (e.g. conventional exploration methods and microtremor array measurements) are considerably less expensive for obtaining shallow velocity structures.
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This result indicates that the excitation of the basin-induced fundamental Love wave is strongly characterized by the shallow sedimentary velocity structure, irrespective of the bedrock depth.
These zones are caused by the existence of shallow low velocity zones and are a problem to interpretation efforts in the South Caspian Sea.
In shallow flows, velocity estimation using tracers entails considerable uncertainty and caution must be taken with these measurements, especially in field studies where these variables vary appreciably in space and time.
In this work we present P and S receiver function results that detect a shallow negative velocity contrast in the mantle below the Eastern Alps and its depth variations that occur over length scales of several tens of kilometers.
They found that the slip is small for the high-velocity regions and large in the shallow low-velocity regions, and concluded that crustal structure heterogeneity could control the rupture process of the mainshock.
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