A ProvÃncia AurÃfera TapajÃ³s-Xingu: AvanÃ§os no ... - ADIMB

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De La Roche et al. (1980)
Page 1 and 2: A Província Aurífera Tapajós-Xin
Page 4 and 5: THE UATUMÃ MAGMATISMIncludes calc-
Page 6: 1.9 - 1.86 MAGMATIC-HYDROTHERMAL MI
Page 9: Schematic stratigraphy of the Tapaj
Page 12 and 13: Au high-sulfidationmineralizationCu
Page 14 and 15: Schematic cross-section of the high
Page 16 and 17: AluniteJuliani et al. (2005)Paleopr
Page 18 and 19: Pyrite sulfur isotopeTapajós HS: -
Page 20 and 21: The low-sulfidation (adularia-seric
Page 22 and 23: Stratigraphy of volcanicrocks and p
Page 24 and 25: Rhyolites strongly affected by adul
Page 26 and 27: Quartz and sulfide veins in strongl
Page 30: Xingu areaLagler (2011)Juliani & Fe
Page 33: Ash tuffSpherulitesMarine calciaren
Page 37: Not all rocks interpreted as A-type
Page 41 and 42: Porphyry-like deep emplaced Au gran
Page 43 and 44: Palito mine geologyN1 km
Page 45: Hydrothermal alteration in the Pali
Page 51: Massive sulfide vein with chalcopyr
Page 54 and 55: Echeverri-Misas (2010)Biotite
Page 56 and 57: SULFUR ISOTOPICCOMPOSITIONMineralδ
Page 60: PhanerozoicbasinHS mineralization
Page 66 and 67: Geologic environment in the Paleopr
Page 70: Tassinari & Macambira (1999) Santos
Page 75: At least 2magmatic arcs ?ANPJuruena
Page 88 and 89:
Are the Tapajósprovince and Tapaj
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A ProvÃncia AurÃfera TapajÃ³s-Xingu: AvanÃ§os no ... - ADIMB