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![](./images/clear.gif) 1.- COLLAPSE KINK STRUCTURE AND ITS CONTRIBUTION TO THE FORMATION OF THE SUPERGENE IRON ORES AND TO THE DEVELOPMENT OF THE CAINOZOIC BASINS AT THE QUADRILATERO FERRIFERO, MINAS GERAIS, BRAZIL
[INTERNATIONAL GEOLOGICAL CONGRESS]; [LOCATION VARIES]; III; INTERNATIONAL, 2000
BRAZIL 2000; 31ST INTERNATIONAL GEOLOGICAL CONGRESS; ABSTRACT VOLUME
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