PROBLEMS OF SIDERITE FORMATION AND IRON ORE EPOCHS: COMMUNICATION 1. TYPES OF SIDERITE-BEARING IRON ORE DEPOSITS

dc.contributor.author	Kholodov V.N.
dc.contributor.author	Butuzova G.Yu.
dc.date.accessioned	2022-09-28T05:54:13Z
dc.date.available	2022-09-28T05:54:13Z
dc.date.issued	2004
dc.identifier	https://elibrary.ru/item.asp?id=13461102
dc.identifier.citation	Lithology and Mineral Resources, 2004, 39, 5, 389-411
dc.identifier.issn	0024-4902
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38798
dc.description.abstract	It is shown that siderite is unstable during sedimentation, diagenesis, and metamorphism of sedimentary and volcanosedimentary rocks. Regularities in the distribution of siderite in Precambrian jaspilites (iron formations), metasomatic ores of the Bakal type, continental–marine coaliferous formations, and oolitic iron ores are discussed. The genesis of the Precambrian iron formations and Riphean–Lower Paleozoic elisional–hydrothermal deposits is considered. The genetic relation of nodular siderites from coaliferous formations and oolitic iron ores with lowmoor coal-forming peat deposits is noted.
dc.title	PROBLEMS OF SIDERITE FORMATION AND IRON ORE EPOCHS: COMMUNICATION 1. TYPES OF SIDERITE-BEARING IRON ORE DEPOSITS
dc.type	Статья

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