H. Nouze et al., PASISAR - PERFORMANCES OF A HIGH AND VERY HIGH-RESOLUTION HYBRID DEEP-TOWED SEISMIC DEVICE, Marine geophysical researches, 19(5), 1997, pp. 379-395
The Pasisar seismic acquisition system combines a source at the sea su
rface and a deep-towed single channel streamer. This unconventional de
vice geometry reduces the width of the first Fresnel zone which increa
ses the lateral resolution. However. the device acquisition geometry g
enerates artifacts on seismic profiles and induces large incidence ang
les of the seismic signal. A specific processing sequence must be appl
ied to the data to obtain a readable seismic section. Penetration of t
he seismic signal depends on the energy of the signal reaching the sea
floor and on its incidence angle. Because of smaller source energy. 80
0 Joules Sparker data cannot be acquired in water depth larger than 15
00 m for example, whereas there is no depth limit for the use of this
system with air gun sources. Differential acoustic absorption of seism
ic frequencies (below 1000 Hz) in the water column is negligible when
compared with wave fronts expansion. Thus, the horizontal resolution o
f any seismic system strongly depends on the frequency spectrum of the
seismic source and on the travel distances. Pasisar and conventional
seismic profiles being usually simultaneously recorded, we illustrate
the interest of using a hybrid seismic device by comparing horizontal
resolutions as well as sipnal-to-noise ratio obtained with both the Pa
sisar and conventional systems. In addition, by carefully picking time
arrivals of a reflection on simultaneously recorded surface and deep-
towed seismic records, it is possible to estimate the average interval
seismic velocity. We present the simplified example of a horizontal r
eflector.