"Sediment budget in a deep-sea core from the central equatorial Pacific" by G. Ross Heath, Theodore C. Moore Jr. et al.
 

Abstract

Stratigraphic, mineralogic, chemical, and geochronologic measurements on a core from 8°20'N, 153°W show that sediment has been accumulating at a rate of 160 g/cm2/106 years. Of this, 125 g is "fresh" Quaternary sediment while the remainder is lower and middle Tertiary material eroded from nearby outcrops....

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