Journal Title
Title of Journal: Min Dep
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Abbravation: Mineralium Deposita
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Publisher
Springer-Verlag
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Authors: Charles H Thorman Ed DeWitt Marcos A Maron Eduardo A Ladeira
Publish Date: 2001/05/19
Volume: 36, Issue: 3-4, Pages: 218-227
Abstract
Brazil has been a major but intermittent producer of gold since its discovery in 1500 Brazil led the world in gold production during the 18th and early 19th centuries From the late 19th century to the late 20th century total mining company and garimpeiro production was small and relatively constant at about 5 to 8 t/year The discovery of alluvial deposits in the Amazon by garimpeiros in the 1970s and the opening of eight mines by mining companies from 1983 to 1990 fueled a major boom in Brazils gold production exceeding 100 t/year in 1988 and 1989 However garimpeiro alluvial production decreased rapidly in the 1990s to about 10 t/year by 1999 Company production increased about tenfold from about 4 t/year in 1982 to 40 t in 1992 Production from 1992 to the present remained relatively stable even though several mines were closed or were in the process of closing and no new major mines were put into production during that periodBased on their production history from 1982–1999 17 gold mines are ranked as major 20 t and minor 3–8 t mines From 1982–1999 deposits hosted in Archean rocks produced 66 of the gold in Brazil whereas deposits in Paleoproterozoic and Neoproterozoic rocks accounted for 19 and 15 respectively Deposits in metamorphosed sedimentary rocks especially carbonaterich rocks and carbonate ironformation yielded the great bulk of the gold Deposits in igneous rocks were of much less importance The Archean and Paleoproterozoic terranes of Brazil largely lack basemetalrich volcanogenic massive sulfide deposits porphyry deposits and polymetallic veins and sedimentary exhalative deposits An exception to this is in the Carajás Mineral Province
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Other Papers In This Journal:
- Some primary structures in the chromitites of Orissa, India
- Vein graphite deposits: geological settings, origin, and economic significance
- Marymia: an Archean, amphibolite facies-hosted, orogenic lode-gold deposit overprinted by Palaeoproterozoic orogenesis and base metal mineralisation, Western Australia
- The Nolans Bore rare-earth element-phosphorus-uranium mineral system: geology, origin and post-depositional modifications
- New isotopic evidence bearing on bonanza (Au-Ag) epithermal ore-forming processes
- The jacupirangite at Kodal, Vestfold, Norway
- 40 Ar/ 39 Ar and K–Ar geochronology of magmatic and hydrothermal events in a classic low-suphidation epithermal bonanza deposit: El Peñon, northern Chile
- New age metals: the geology and genesis of ores required for a changing economy and a carbon-constrained world—preface to a thematic issue on critical commodities
- Hypogene Zn carbonate ores in the Angouran deposit, NW Iran
- Nd-Sr-Pb isotopic constraints on metal and fluid sources in W-Sb-Au mineralization at Woxi and Liaojiaping (Western Hunan, China)
- High-grade iron ore at Windarling, Yilgarn Craton: a product of syn-orogenic deformation, hypogene hydrothermal alteration and supergene modification in an Archean BIF-basalt lithostratigraphy
- A comparison of progressive hydrothermal carbonate alteration in Archean metabasalts and metaperidotites
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