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2Physical Properties of Marine SedimentsFig. 2.23 Parasound seismogram section recorded across an inactive meandering channel in the Bengal Fan. The sediments of the terrace were sampled by pistoncore 47KL marked by the black bar. Vertical exaggeration (VE) of sedimentary structures is 200. The ship’s course is displayed above the seismogram section. Theterrace exhibits features which might be interpreted as old buried channels. Modified after Breitzke (1997).62
2.6 Sediment EchosoundingFig. 2.24 Coring site of 47KL. From left to right: Enlarged part of the Parasound seismogram section recorded on approaching site 47KL. Comparison of syntheticseismograms computed on basis of P-wave velocity and wet bulk density measurements on 47KL with Parasound seismograms recorded at the coring site. Physicalproperties and age model of piston core 47KL. Wet bulk densities, carbonate content and oxygen isotope stratigraphy (G. ruber pink) are taken from (Kudrass 1994,1996). Modified after Breitzke (1997).63
Page 3 and 4: 2.2 Porositiy and Wet Bulk Densityi
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Page 17 and 18: 2.4 Acoustic and Elastic Properties
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Page 39 and 40: AppendixFig. 2.25 a, b Parasound se
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Page 43 and 44: References2.7 ProblemsProblem 1What
Page 45: Referencespressional wave in a poro

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