Phosphate Deposits of the World Volume 3 Neogene to Modern Phosphorites

This book PDF is perfect for those who love Science genre, written by P. J. Cook and published by Cambridge University Press which was released on 23 June 1986 with total hardcover pages 486. You could read this book directly on your devices with pdf, epub and kindle format, check detail and related Phosphate Deposits of the World Volume 3 Neogene to Modern Phosphorites books below.

Phosphate Deposits of the World  Volume 3  Neogene to Modern Phosphorites
Author : P. J. Cook
File Size : 53,9 Mb
Publisher : Cambridge University Press
Language : English
Release Date : 23 June 1986
ISBN : 0521333709
Pages : 486 pages
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Phosphate Deposits of the World Volume 3 Neogene to Modern Phosphorites by P. J. Cook Book PDF Summary

The origin of marine phosphorites, the principal raw material for phosphatic fertilizers, appears to be related mainly to marine biological productivity, often associated with upwelling currents during certain intervals of geological time. This book examines the environmental setting and resulting phosphorites which formed during the Miocene period, and investigations of modern oceanic environments where phosphorites are presently forming are also described.

Phosphate Deposits of the World  Volume 3  Neogene to Modern Phosphorites

The origin of marine phosphorites, the principal raw material for phosphatic fertilizers, appears to be related mainly to marine biological productivity, often associated with upwelling currents during certain intervals of geological time. This book examines the environmental setting and resulting phosphorites which formed during the Miocene period, and investigations of

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Phosphate Deposits of the World

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Phosphatic concretions occur within diatomite in the upper part of the Miocene Monterey Formation near Lompoc, Calif. Absence of disruption of fine laminar bedding in the associated sediment by the concretions shows that they formed after complete compaction of the enclosing sediment.The concretions exhibit a strongly concentric color, chemical,

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