Archaean mafic magmatism in the Kalgoorlie area of the Yilgarn Craton, Western Australia: A geochemical and Nd isotopic study of the petrogenetic and tectonic evolution of a greenstone belt

Precambrian Research

Volumn 108, Issue 1-2, 2001, Pages 75-112

  Bateman, Roger ^a   Costa, Sylvie ^b   Swe, Theingi ^c   Lambert, David ^b  

^a Kalgoorlie Consolidated Gold Mines   (Australia)

^b MONASH UNIVERSITY   (Australia)

^c St Barbara Limited   (Australia)

Author keywords

Basalt; Contamination; Fractionation; Gabbro; Komatiite; Trace elements

Indexed keywords

ISOTOPE; LANTHANIDE; MINERAL; NEODYMIUM; TRACE ELEMENT;

ARCHEAN; CRATON; GREENSTONE BELT; MAGMATISM; PETROGENESIS; TECTONIC EVOLUTION;

ARTICLE; AUSTRALIA; EVOLUTION; FRACTIONATION; GEOLOGY; ROCK; VOLCANO;

AUSTRALIA;

EID: 0035340202     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0301-9268(00)00148-0     Document Type: Article

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12. The Sm-Nd age of Kambalda volcanics is 500 Ma too old!
13. Sources of error in external calibration ICP-MS analysis of geological samples and an improved non-linear drift correction procedure
14. Geology of the Kalgoorlie gold field
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35. Precambrian history of the West Australian craton and adjacent areas
36. Preface: Archaean geology of the Eastern Goldfields of Western Australia: Regional overview
37. Evolution of the Archaean granite-greenstone terranes of the Eastern Goldfields. Western Australia: SHRIMP U-Pb zircon constraints
38. X-ray fluorescence spectrometry
39. Majorite fractionation and genesis of komatiite in the deep mantle
40. Partitioning of elements between majorite garnet and melt: Implications for petrogenesis of komatiites
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52. Low pressure experimental constraints on the evolution of komatiites
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