lWe analyse the geophone orientation and coupling in a data set from the No
rth Sea. Based on the polarization of the water-break on the sea-floor, we
have derived processing algorithms for determining the receiver orientation
for gimballed and non-gimballed geophone systems. For a gimballed system,
the problem reduces to a simple horizontal rotation. However, for a non-gim
balled system, where all three geophone axes may vary due to varying acquis
ition conditions such as dipping sea-floor, twisting of recording cable, et
c., the three orientation angles cannot be found directly from the recorded
displacement vectors. Using the data redundancy within a common-receiver g
ather, a robust two-stage method is derived for the non-gimballed system in
which all three orientations can initially be unknown. Testing on the Nort
h Sea data set acquired with a gimballed system shows that the three-compon
ent geophones in the data set are orientated satisfactorily within an error
of 5 degrees. However, there are some undesirable cross-couplings between
the vertical and horizontal geophones, which results in leakage of shear-wa
ve energy from the horizontal components to the vertical components.