Ww. Sager et al., High-frequency near-bottom acoustic reflection signatures of hydrocarbon seeps on the Northern Gulf of Mexico continental slope, GEO-MAR LET, 18(4), 1999, pp. 267-276
Acoustic reflection signatures of four hydrocarbon seeps were classified us
ing near-bottom 25-kHz echosounder profiles. Echo patterns were compared wi
th ground-truth data obtained by submersible observations and shallow corin
g. Six echo types were distinguished: strong reflections from (1) exposed o
r (2) buried hard substrates, such as authigenic carbonate or gas hydrate;
acoustic scattering in (3) unlayered or (4) layered sediments owing to gas,
shells, or disseminated carbonates; (5) attenuation caused by gas; and (6)
undisturbed sediments. Echo type distributions suggest that high spatial v
ariability indicates a younger, vigorous seep, whereas extensive hard subst
rate implies an older, encrusted seep.