In many physical phenomena, the laws governing motion can be looked at as t
he relationship between unified dual fields which are continuous in time an
d space. Both fields are activated by a single source. The most notable exa
mple of such phenomena is electromagnetism, in which the dual fields are th
e electric field and the magnetic field. Another example is acoustics, in w
hich the dual fields are the particle-velocity field and the pressure field
. The two fields are activated by the same source and satisfy two first-ord
er partial differential equations, such as those obtained by Newton's laws
or Maxwell's equations. These equations are symmetrical in time and space,
i.e., they obey the same wave equation, which differs only in the interface
condition changing sign. The generalization of the Einstein velocity addit
ion equation to a layered system explains how multiple reflections are gene
rated. This result shows how dual sensors at a receiver point at depth prov
ide the information required for a new deconvolution method. This method is
called Einstein deconvolution in honor of Albert Einstein. Einstein deconv
olution requires measurements of the pressure signal, the particle velocity
signal, and the rock impedance, all at the receiver point. From these meas
urements, the downgoing and upgoing waves at the receiver are computed. Ein
stein deconvolution is the process of deconvolving the upgoing wave by the
downgoing wave. Knowledge of the source signature is not required. Einstein
deconvolution removes the unknown source signature and strips off the effe
cts of all the layers above the receiver point. Specifically, the output of
Einstein deconvolution is the unit-impulse reflection response of the laye
rs below the receiver point. Compared with the field data, the unit-impulse
reflection response gives a much clearer picture of the deep horizons, a d
esirable result in all remote detection problems. In addition, the unit-imp
ulse reflection response is precisely the input required to perform dynamic
deconvolution. Dynamic deconvolution yields the reflectivity (i.e., reflec
tion-coefficient series) of the interfaces below the receiver point. Altern
atively, predictive deconvolution can be used instead of dynamic deconvolut
ion.