Hi all and apologies for x-posting.
A quick but provocative query:
is there any documented study of the transmissivity, even far (80/100+
km) from the seismogenic source, of P-waves and damage on competent,
consistently thick (6/7 km, from subsurface data) carbonate platforms?
In other words, how much can felt reports from a major seismic event
cluster on terrains pertaining to an outcropping major foreland?
Many thanks for any hint and have a pleasant day,
Ciao,
Umberto
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Umberto Fracassi
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Istituto Nazionale di Geofisica e Vulcanologia
Via di Vigna Murata, 605
00143 Roma
Italy
Tel: +39-06-51860557
Fax: +39-06-5041181
Email: [log in to unmask]
WWW: http://www.ingv.it/paleo/fracassi/
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"This is what you should do: Love the earth and the sun and the animals, despise riches, give alms to everyone that asks, stand up for the stupid and crazy, devote your income and labor to others, hate tyrants, argue not concerning god, have patience and indulgence toward people, take off your hat to nothing known or unknown, or to anyone or number of people ....reexamine all you have been told at school or church, or in any book, dismiss what insults your soul, and your very flesh shall be a great poem."
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