Redox state of the Archean atmosphere: Evidence from detrital heavy minerals in ca. 3250-2750 Ma sandstones from the Pilbara Craton, Australia

Geology

Volumn 27, Issue 2, 1999, Pages 115-118

  Rasmussen, Birger ^a   Buick, Roger ^b  

^a UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

^b UNIVERSITY OF SYDNEY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

CLAY ALTERATION; OXIDE MINERALS; PHOSPHATE MINERALS; PYRITES; SILICATE MINERALS; TITANIUM DIOXIDE; WATER AERATION; ZIRCON;

ATMOSPHERIC OXYGEN; HEAVY MINERALS; HYDROTHERMAL ALTERATIONS; OXIDIZING ENVIRONMENTS; REDOX SENSITIVES; REDUCED SULFUR SPECIES; SILICICLASTIC SEDIMENTS; WITWATERSRAND;

SANDSTONE;

ARCHEAN; ATMOSPHERIC CHEMISTRY; HEAVY MINERAL; REDOX CONDITIONS;

AUSTRALIA; PLIBARA CRATON; WESTERN AUSTRALIA;

EID: 84874954159     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1999)027<0115:RSOTAA>2.3.CO;2     Document Type: Article

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