. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. SECT. 3] CLAY-MINERAL DISTRIBUTIONS IN THE PACIFIC OCEAN 737 decreasing in intensity with concomitant increase in intensity and resolution of the ilHte and chlorite peaks would lead one to believe that the 17 A material was transforming to a well crystallized illite and chlorite. Undoubtedly this is one of the factors that is influencing the clay-mineral distribution pattern in the a & 4,7a 5& 1 I 7I& 10 S I7&. CK22 ZS'aa'N 168*53 W ' V\**Vyy^/W MP 40-1 16° N 178° E. Please note that these images ar
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. SECT. 3] CLAY-MINERAL DISTRIBUTIONS IN THE PACIFIC OCEAN 737 decreasing in intensity with concomitant increase in intensity and resolution of the ilHte and chlorite peaks would lead one to believe that the 17 A material was transforming to a well crystallized illite and chlorite. Undoubtedly this is one of the factors that is influencing the clay-mineral distribution pattern in the a & 4,7a 5& 1 I 7I& 10 S I7&. CK22 ZS'aa'N 168*53 W ' V\**Vyy^/W MP 40-1 16° N 178° E. 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
