Özet
We locate the concealed Carlsberg Fault zone in the city of Copenhagen from seismic fan recordings. The fault is part of a fault system close to the border between the Danish Basin and the Baltic Shield. Recent earthquakes indicate that this area is tectonically active. The fault zone is a seismic low-velocity zone. Fan shots were recorded on three receiver arrays (1.5-2.4 km long arcs) across the fault. Sources were placed inside and up to ∼500 m away from the ∼400-700 m wide fault zone at offsets of up to ∼7 km. Shots inside the fault zone show: 1) weak, delayed first arrivals inside the fault zone; 2) stronger first arrivals outside the fault zone; 3) guided waves inside the fault zone. The fault is a shadow zone for shots detonated outside the fault zone. Our approach facilitates fault mapping in densely urbanized areas where seismic profiling is not feasible.
Orijinal dil | İngilizce |
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Sayfa (başlangıç-bitiş) | L07621 1-4 |
Dergi | Geophysical Research Letters |
Hacim | 31 |
Basın numarası | 7 |
DOI'lar | |
Yayın durumu | Yayınlandı - 16 Nis 2004 |
Harici olarak yayınlandı | Evet |