. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Fig. 24. Relative tx'ade-wind intensity as a function of geological time. The relative intensity is esti- mated from the ensuing productivity changes at the Equatorial Diverg- ence. (From Arrhenius, 1952.) PELAGIC SEDIMENTS — AEOLIAN DUST 1 2 3 4 6 8 10 20 40 particle size yL, Fig. 25. Particle-size distribution in pelagic sediments from the North Pacific and in eolian dust from Illinois. (Data from Rex, 1958; Udden, 1914.) investigation by Peterson and Goldberg (1962) shows that such feldspar species prevail over a la
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Fig. 24. Relative tx'ade-wind intensity as a function of geological time. The relative intensity is esti- mated from the ensuing productivity changes at the Equatorial Diverg- ence. (From Arrhenius, 1952.) PELAGIC SEDIMENTS — AEOLIAN DUST 1 2 3 4 6 8 10 20 40 particle size yL, Fig. 25. Particle-size distribution in pelagic sediments from the North Pacific and in eolian dust from Illinois. (Data from Rex, 1958; Udden, 1914.) investigation by Peterson and Goldberg (1962) shows that such feldspar species prevail over a large part of the East Pacific Rise. For the Atlantic, Radczewski (1937) and Leinz (1937) showed that acidic rocks must have been the main source of feldspar in the Cape Verde and the Guinea Basins, inasmuch as the. 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
