This paper reviews the current concepts on petrogenesis of metamorphosed manganese-rich sedimentary rocks with the aim to identify the processes, their various controls and the possible progenitors. On the basis of mineralogical composition, five distinct rock types have been identified which show 21 mineral assemblages in total. Mineralogical, textural and chemical data on naturally occurring phases of these five rock types are also presented. These data, together with the results of experimental studies are used to interpret the metamorphic evolution of the different rock types. Finally, an attempt has been made to determine the possible precursor sediment types
Manganese-bearing minerals in ancient strata provide a particularly informative record of the redox ...
Abstract: Facies analysis of the unmetamorphosed sediments enclosing the stratiform manganese oxide ...
Bibliography: pages 125-130.1. Regional geology -- 2. Paleoenvironment and regional history -- 3. Ma...
Abstract: This paper aims at reviewing the mineralogy, mineral chemistry and petrology of metamorpho...
This paper aims at reviewing the mineralogy, mineral chemistry and petrology of metamorphosed mangan...
The major manganese deposits of the world can be classified into three broad genetic types: hydrothe...
Sedimentary manganese-oxide ores occur interstratified with chert and minor calcareous shale and enc...
The two most important types of manganese deposits in China are sedimentary and super-gene, which ac...
Manganese ore deposits occurred in various types of syngenetic, diagenetic and epigenetic mineraliza...
Until its closure in 1997, the Serra do Navio deposit, located in Amapá Province, Brazil, was one of...
Manganese deposits of the Bharweli area are conformable with the enclosing Precambrian quartzites, p...
Manganese mineral and ore occurrences, the associated underlying ophiolitic rocks of tholeiitic comp...
The destructive type of tectonic regimes directly controlled the formation of the larger part of pri...
Mn silicate-carbonate rocks at Parseoni occur as conformable lenses within metapelites and calc-sili...
The manganese orebodies at Bharweli, Balaghat District, Madhya Pradesh, India, occur conformably wit...
Manganese-bearing minerals in ancient strata provide a particularly informative record of the redox ...
Abstract: Facies analysis of the unmetamorphosed sediments enclosing the stratiform manganese oxide ...
Bibliography: pages 125-130.1. Regional geology -- 2. Paleoenvironment and regional history -- 3. Ma...
Abstract: This paper aims at reviewing the mineralogy, mineral chemistry and petrology of metamorpho...
This paper aims at reviewing the mineralogy, mineral chemistry and petrology of metamorphosed mangan...
The major manganese deposits of the world can be classified into three broad genetic types: hydrothe...
Sedimentary manganese-oxide ores occur interstratified with chert and minor calcareous shale and enc...
The two most important types of manganese deposits in China are sedimentary and super-gene, which ac...
Manganese ore deposits occurred in various types of syngenetic, diagenetic and epigenetic mineraliza...
Until its closure in 1997, the Serra do Navio deposit, located in Amapá Province, Brazil, was one of...
Manganese deposits of the Bharweli area are conformable with the enclosing Precambrian quartzites, p...
Manganese mineral and ore occurrences, the associated underlying ophiolitic rocks of tholeiitic comp...
The destructive type of tectonic regimes directly controlled the formation of the larger part of pri...
Mn silicate-carbonate rocks at Parseoni occur as conformable lenses within metapelites and calc-sili...
The manganese orebodies at Bharweli, Balaghat District, Madhya Pradesh, India, occur conformably wit...
Manganese-bearing minerals in ancient strata provide a particularly informative record of the redox ...
Abstract: Facies analysis of the unmetamorphosed sediments enclosing the stratiform manganese oxide ...
Bibliography: pages 125-130.1. Regional geology -- 2. Paleoenvironment and regional history -- 3. Ma...