Abstract: The Nconga Formation of the Mesoarchean (~2.96–2.84 Ga) Mozaan Group of the Pongola Supergroup of southern Africa contains the world’s oldest known granular iron formation. Three dimensional reconstructions of the granules using micro-focus X-ray computed tomography reveal that these granules are microstromatolites coated by magnetite and calcite, and can therefore be classified as oncoids. The reconstructions also show damage to the granule coatings caused by sedimentary transport during formation of the granules and eventual deposition as density currents. The detailed, three dimensional morphology of the granules in conjunction with previously published geochemical and isotope data indicate a biogenic origin for iron precipitat...
The ca. 1.88 Ga Sokoman continental margin-type iron formation (IF) was studied by detailed mineral-...
Iron formations are typically thinly bedded or laminated sedimentary rocks containing 15% or more of...
Banded iron formations (BIF) are Precambrian sedimentary rocks characterized by alternating iron- an...
Abstract: The Nconga Formation of the Mesoarchean (~2.96–2.84 Ga) Mozaan Group of the Pongola Superg...
Toward the end of the Palaeoproterozoic era, over 109 billion tonnes of banded (BIF) and granular (G...
M.Sc.The Mesoarchean Witwatersrand and Pongola Supergroups of South Africa are the oldest, well pres...
Iron formations (IF) represent an iron-rich rock type that typifies many Archaean and Proterozoic su...
Iron formations are economically significant, iron- and silica-rich sedimentary rocks that are restr...
Precambrian banded iron formations provide an extensive archive of pivotal environmental changes and...
Banded iron formations (BIFs) are sedimentary records of the coevolutionary history of geosphere and...
Iron formations are typically thinly bedded or laminated sedimentary rocks containing 15% or more of...
© 2016 Elsevier B.V.Banded iron formations (BIFs) were deposited as deep-water facies distal to the ...
We constrained the origin and genetic environment of modern iron ooids (sand-sized grains with a cor...
See also "Widespread and persistent deposition of iron formations for two billion years: Compilation...
Problematic microfossils dominate the palaeontological record between the Great Oxidation Event 2.4 ...
The ca. 1.88 Ga Sokoman continental margin-type iron formation (IF) was studied by detailed mineral-...
Iron formations are typically thinly bedded or laminated sedimentary rocks containing 15% or more of...
Banded iron formations (BIF) are Precambrian sedimentary rocks characterized by alternating iron- an...
Abstract: The Nconga Formation of the Mesoarchean (~2.96–2.84 Ga) Mozaan Group of the Pongola Superg...
Toward the end of the Palaeoproterozoic era, over 109 billion tonnes of banded (BIF) and granular (G...
M.Sc.The Mesoarchean Witwatersrand and Pongola Supergroups of South Africa are the oldest, well pres...
Iron formations (IF) represent an iron-rich rock type that typifies many Archaean and Proterozoic su...
Iron formations are economically significant, iron- and silica-rich sedimentary rocks that are restr...
Precambrian banded iron formations provide an extensive archive of pivotal environmental changes and...
Banded iron formations (BIFs) are sedimentary records of the coevolutionary history of geosphere and...
Iron formations are typically thinly bedded or laminated sedimentary rocks containing 15% or more of...
© 2016 Elsevier B.V.Banded iron formations (BIFs) were deposited as deep-water facies distal to the ...
We constrained the origin and genetic environment of modern iron ooids (sand-sized grains with a cor...
See also "Widespread and persistent deposition of iron formations for two billion years: Compilation...
Problematic microfossils dominate the palaeontological record between the Great Oxidation Event 2.4 ...
The ca. 1.88 Ga Sokoman continental margin-type iron formation (IF) was studied by detailed mineral-...
Iron formations are typically thinly bedded or laminated sedimentary rocks containing 15% or more of...
Banded iron formations (BIF) are Precambrian sedimentary rocks characterized by alternating iron- an...