Kholodov,V.N. and Nedumov,R.I.(2009): Association of manganese ore and phosphorite-bearing facies in sedimentary sequences; Communication 1. Parastereses and parageneses of phosphorus and manganese in Mesozoic-Cenozoic and Upper Paleozoic rocks. Lithology and Mineral Resources, 44(1), 1-18.

『堆積層準におけるマンガン鉱石とリン鉱石を含む相の共存:報告1.中生代−新生代および古生代後期岩石中のリンとマンガンの空間的共存と共生』


Abstract
 It is shown that cooccurrences (parastereses) of chemical elements, minerals, sedimentary rocks, facies, and formations should be distinguished from their parageneses, which represent geological formations related to a single geological process. It has been established that phosphorus is concentrated in sedimentary manganese ores and is not accumulated in volcanosedimentary and hydrothermal deposits. Parageneses of Mn and P in sedimentary deposits are characterized. Parastereses of manganese ore and phosphorite-bearing facies in Oligocene rocks of southwestern Eurasia, Mesozoic and Upper Paleozoic sections of the Urals, and Mesozoic-Cenozoic sequences of Morocco are considered.』

(Introduction)
Regularities of phosphorus distribution in the Upper Paleozoic, Mesozoic, and Cenozoic sedimentary manganese deposits
Cooccurrence of manganese ore and phosphorite-bearing facies in Upper Paleozoic and Mesozoic-Cenozoic sequences
Association of different phosphorite deposits with sedimentary manganese deposits
Conclusions
acknowledgments
References


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