Historical Seismicity and Present-Day Microearthquake Activity of the Rhenish Massif, Central Europe
作者： L. Ahorner
DOI: 10.1007/978-3-642-69219-2_27
关键词:
摘要: The earthquake activity of the Rhenish Massif, which has undergone some 300 m plateau uplift since Late Tertiary, is analyzed. Seismotectonic implications on geodynamic processes controlling crustal are discussed. study based a detailed investigation historical seismicity pattern 1500 A.D., and special microearthquake survey carried out during period 1976–1982. A local station network consisting high-sensitive analog or digital recording seismographs been installed in an area about 200 × km2 with average spacing 40 km. More than 800 earthquakes tectonic origin, ranging magnitude from ML = 0 to 4.7, were recorded 6-year study. Most them could be located reasonable accuracy (±1 km horizontally ±2 vertically). Fault-plane solutions derived, general, for shocks magnitudes greater 3.
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