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Zusammenfassung:
Natural hazard prediction and efficient crust exploration require dense seismic observations in time and space.
Seismological techniques provide ground-motion data, whose accuracy depends on sensor capacity and distribu-
tion. More and denser networks are being deployed on volcanoes, sedimentary areas in order improve of capability
to image and monitor the crust. It has been suggested for some months that fibre optic cable technology is able
to record strain and is useful in industry related exploration and may be useful for seismology. We review the
distributed Sensing technologies for such applications.
In this study, we demonstrate that direct strain determination is now possible with conventional fibre-optic
cables deployed for telecommunication and is a new tool for earthquake location, for crustal exploration using
unexpected sources and provides key records for understanding earthquake and fault structure and behaviour.
Extending recently distributed acoustic sensing (DAS) studies, we provide spatially un-aliased broadband nano-
strain data. We record seismic signals from natural and man-made sources with 4-m spacing along a 15-km-long
fibre-optic cable layout on Reykjanes Peninsula, SW Iceland. We identify with unprecedented resolution structural
features like normal faults and dykes in the Reykjanes Oblique Rift, allowing to infer new fault dynamic processes.
Comparison with conventional seismometer recordings corroborates dynamic and stable spectral amplitudes
between 0.1-100 Hz bandwidth. The networks of fibre-optic telecommunication lines worldwide may be used as
seismometers opening a new window for Earth hazard monitoring and exploration.
