Rd. Muller et al., SEABED CLASSIFICATION OF THE SOUTH TASMAN RISE FROM SIMRAD EM12 BACKSCATTER DATA USING ARTIFICIAL NEURAL NETWORKS, Australian journal of earth sciences, 44(5), 1997, pp. 689-700
We have developed an automated method for sea-floor classification for
the South Tasman Rise, based on a SIMRAD EM12-backscatter (13 kHz) mo
saic and 47 sea-floor samples. The samples have been divided into 3 di
stinct groups representing: (i) thick blankets of foraminiferal ooze;
(ii) mixed sediments comprising sand/silt/mud (turbidites/chalk); and
(iii) outcrops of metamorphic basement and volcanic rocks. A total of
515 sub-areas, each measuring 32x32 pixels (similar to 4 km(2)) and re
presenting the different seabed types, were extracted from the image f
rom areas 128x128 pixels large, centred on the sample locations. The t
exture of the sub-images was analysed by calculating grey-level run-le
ngth features, spatial grey-level dependence matrices, and grey-level
difference vectors in four directions. A total of 100 samples for each
class and 18 feature statistics were chosen to train an artificial ne
ural network to recognise the textural attributes and their variabilit
y for each class. The performance of the network was evaluated first b
y classifying the image sub-areas used for training, followed by class
ification of the remaining sub-areas. Classification accuracies for th
e training samples for ooze, sand/silt/mud and basement rocks are 98%,
98% and 91%, respectively, and 91%, 83% and 84% for the test samples.
Subsequently, we classified a total of more than 20 000 unknown image
sub-areas 4 km(2) large on the northern South Tasman Rise. The result
agrees well with a visual geological interpretation of the sidescan m
osaic as well as with a facies map of the area based on 3.5 kHz data.
The success of a combined textural image and neural network analysis t
o classify a sidescan mosaic, in the presence of noise and processing
artifacts, suggests a wide range of potential applications including t
he recognition of sediment textures and other objects in high-resoluti
on, shallow-water backscatter images, and pattern recognition in remot
ely sensed geophysical images for mineral exploration.