Abstract
Beginning about a decade ago [1], the appreciation of the need for broadband data with a high dynamic range from globally distributed stations has led the seismological community to undertake several initiatives. Examples are the GEOSCOPE, IRIS/IDA, IRIS/USGS, MedNet and GEOFON networks, complemented by national efforts, such as in China, Canada or Mexico. All these groups co-operate in co-ordinating station deployment and data exchange within the framework of the Federation of Digital Seismographic Networks (FDSN; [2]). There are now 80–100 operational stations with the very-broad-band response (0.2-360 seconds) and dynamic range up to 140 db that meet the FDSN Network requirements. Their geographical distribution is yet far from the optimal, with only 25% of the stations located in the Sorthern Hemisphere and with the vast unoccupied oceanic areas.
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Dziewonski, A.M., Ekström, G., Liu, XF. (1996). Structure at the Top and Bottom of the Mantle. In: Husebye, E.S., Dainty, A.M. (eds) Monitoring a Comprehensive Test Ban Treaty. NATO ASI Series, vol 303. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0419-7_28
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DOI: https://doi.org/10.1007/978-94-011-0419-7_28
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