Seismic Travel Time 1D

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Description

Travel time from source to reciever in 1D local model.

Usage

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travel.time1D(indelta, inhpz, instaz, inlay, ztop, vel)
many.time1D(indelta, inhpz, instaz, inlay, ztop, vel)

Arguments

indelta

distance in KM

inhpz

depth of hypocenter, km

instaz

elevation of station

inlay

number of layers

ztop

vector, tops of layers

vel

vector, velocities in layers

Details

Uses local 1D velocity model, not appropriate for spherical earth. The many.time1D version will take a vector of distances (indelta) and either one station elevation or a vector.

The station elevation should be referenced to the top of the velocity model, not necessarily sea level. Usually this is set to zero and a station correction is used to take into account the topographic and other geologic effects.

Value

list:

dtdr

derivative of t w.r.t. horizontal distance

dtdz

derivative of t w.r.t. z, depth

angle

incidence angle, degrees

tt

travel time, s

Author(s)

Jonathan M. Lees<jonathan.lees.edu>

See Also

Ray.time1D, Get1Dvel

Examples

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data(VELMOD1D)

v <- VELMOD1D

tees <- travel.time1D(23, 7, 0, length(v$zs) , v$zp , v$vp)

print(tees)

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