『Abstract
Different hypotheses of phosphorite formation are discussed.
The biogenic origin of phosphorites is most plausible. The important
role of terrigenous material in P2O5 migration and concentration in the hypergenesis
zone is emphasized. The mineralogical zoning of phosphate accumulations
is described and the probable diagenetic alteration of accessory
apatite in present-day seas and lakes is affirmed.』
(Introduction)
Accessory apatite in the sedimentary process
Zonal distribution of apatite and phosphate minerals in drainage
areas and terminal basins
Conclusions
Acknowledgments
References