. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 100 X 10"" - (a) 10 - - (S^^_-^-*^ - - Galapagos areo^<'^ \ Centrol Equatorial ^^ ^^ - carbonate tccies^^ -^Ap-^ - ""^ ^/ -Tertiary cloy facies M^;^^^^) - m { Tertiary carbonate \ /^pleistocene X. y Clay tacies - fades ^â ^""^ 1 J 1â1â1â1 .. , , 1 1 1 1 1 10 X10"^ N. Fig. 34. Influence of origin and diagenesis on the composition of organic matter (a) in sediment cores with location shown in (b). The distribution is based on approximately 2000 analyses. The envelopes in (a) enclose the
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 100 X 10"" - (a) 10 - - (S^^_-^-*^ - - Galapagos areo^<'^ \ Centrol Equatorial ^^ ^^ - carbonate tccies^^ -^Ap-^ - ""^ ^/ -Tertiary cloy facies M^;^^^^) - m { Tertiary carbonate \ /^pleistocene X. y Clay tacies - fades ^â ^""^ 1 J 1â1â1â1 .. , , 1 1 1 1 1 10 X10"^ N. Fig. 34. Influence of origin and diagenesis on the composition of organic matter (a) in sediment cores with location shown in (b). The distribution is based on approximately 2000 analyses. The envelopes in (a) enclose the central 90% of the total number of samples from the respective areas. (After Arrhenius, 1952.). Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
