On Sat, 12 Aug 2000 sean@........... wrote: > I have never heard of a Pb phase, either in regional or teleseismic > studies. I have no idea what Winquake is doing. Same here, I even asked a few seismo guys...no idea what Pb is. I looked through a few books I have, still no idea. There is a spectrum of possible phases going from the more well known teleseismic phases to Pg etc. to other less known phases the closer the station gets to the source. Perhaps it is an exploration seismo term? Some of the regional complications exist due to a mid-crustal discontinuity. This discontinuity represents the depth (pressure and temperature) where lighter granitic materials transform to denser mineral phases (such as garnet). The depth to this boundary varies as a function of the age, composition, thermal gradient, and thickness of continental crust (which are all in turn inter-related). Also, a sinking of subsiding portion of crust may have a lower boundary than expected, because the reactions that take place to form the denser materials are "kinetically inhibited," meaning that although they are at the right pressure the temperature has not yet risen high enough to give the vibrating atoms enough energy to assume the new crystal geometry. Likewise, an uprising portion of crust may have a higher boundary than expected, because garnet and many other high pressure phases from the mid-crust are stable at the surface. At an even smaller level, many areas contain a "great unconformity" where the initial magmatic rocks which formed the continent are overlain by younger sediments usually along a some what flat surface of ancient erosion. This feature can be observed in some areas, such as the grand canyon in AZ. This will also affect the behavior of waves in certain regions. In general, sediments are seismically slower than magmatic rocks. When some waves travel along the underside of the interface it slowly turns wave fronts up into the sediments. Because the waves slow down while in the sediment, the energy per unit volume increases, which increases the amplitudes. Anyways, this was one of the places I was directed to look into if there really was a Pb phase. If that is the case, its behavior would be quite variable. Maybe the exploration seismo literature would be more relevant? Good Luck! ****************************************************************************** John Hernlund Department of Geological Sciences Arizona State University E-mail: hernlund@....... WWW: http://www.public.asu.edu/~hernlund/ ****************************************************************************** __________________________________________________________ Public Seismic Network Mailing List (PSN-L)
Larry Cochrane <cochrane@..............>