کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4695153 | 1636962 | 2006 | 9 صفحه PDF | دانلود رایگان |
![عکس صفحه اول مقاله: Shear wave splitting in the Eastern Alps observed at the TRANSALP network Shear wave splitting in the Eastern Alps observed at the TRANSALP network](/preview/png/4695153.png)
Data from the temporary TRANSALP seismic network were analysed to investigate the seismic anisotropy in the upper mantle beneath the Eastern Alps. We operated mostly short period and some broadband stations in a dense linear array, which transects the Eastern Alps at ∼12° E longitude. Recorded SKS and SKKS phases with different backazimuths were used simultaneously to calculate the splitting parameters of delay time and fast axis direction for each seismic station. While we found variations in the delay times between ∼0.8 and 2.0 s, the determined fast axis directions prove to be rather consistent along the profile (60°–70° N). They coincide well with the trend of the Eastern Alps, thus suggesting orogen-parallel flow in the upper mantle. Our findings support the earlier proposed idea that the Adriatic indenter which was forced northwards into the European plate during the late stage of the Alpine orogeny, triggered an escape movement to the less constrained Pannonian basin to the east.
Journal: Tectonophysics - Volume 414, Issues 1–4, 23 February 2006, Pages 117–125