. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 670 ARRHENTUS [chap. 25 due to substitution in rutile. The origin of the titanium oxide minerals is still uncertain; it appears probable that the rutile is terrigenous but the anatase might develop in situ (cf. Correns, 1937, 1954; Teodorovich, 1958). The ferromanganese nodules range in size from a few microns, suspended in the sediment or coating other minerals, to intergrowths forming slabs several meters wide. The nodules have alternating growth zones of high and low. Please note that these images are extracted from sca
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 670 ARRHENTUS [chap. 25 due to substitution in rutile. The origin of the titanium oxide minerals is still uncertain; it appears probable that the rutile is terrigenous but the anatase might develop in situ (cf. Correns, 1937, 1954; Teodorovich, 1958). The ferromanganese nodules range in size from a few microns, suspended in the sediment or coating other minerals, to intergrowths forming slabs several meters wide. The nodules have alternating growth zones of high and low. 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
