• Title/Summary/Keyword: Jujuy

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Survey of Borate deposit in Northern Argentina: Salinas Grandes Borate deposit (북부 아르헨티나 붕산염 광상 조사: 살리나스그란데스 광상을 중심으로)

  • Pak, Sang-Joon; Lee, Han-Yeang
    • Journal of the Korean earth science society
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    • v.30 no.7
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    • pp.801-809
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    • 2009
  • The Salinas Grandes borate deposit located in Jujuy state, northern Argentina can be categorized into the playatype evaporite deposit. Major borate mineral is ulexite ($NaCaB_5O_9{\cdot}H_2O$), which boron could be originated from volcanic rocks nearby playa. The eastern part of the Jujuy state in northern Argentina belongs to the Altiplano-Puna platform which shows high altitude and semiarid climate. Lots of Mesozoic and Cenozoic volcanics that are source of boron as well as playas that are the basin for borate precipitation in the area are essential for boron evaporite deposit. Therefore, the extensive explorations for the playa-type evaporite deposit are need.

Field Study of Zapla Iron Ore Deposit in Argentina (아르헨티나 자플라 철광상 현지 조사 연구)

  • Pak, Sang-Joon;Lee, Han-Yeang
    • The Journal of the Petrological Society of Korea
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    • v.18 no.4
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    • pp.307-314
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    • 2009
  • Zapla iron ore bodies in Jujuy state, northern Argentina are located within Paleozoic Silurian marine sedimentary rocks and can be categorized into ironstone deposit. Iron ores contain oolitic hematite as main iron mineral as well as siderite and chamosite. Hematite replaced biotite and/or muscovite along their cleavage or grain boundary, which indicates hematite is precipitated by chemical reaction. Silurian basins in northern Argentina has high potential resources for ironstone deposit but economic aspects of ore body can be controlled by magnitude of lateral vertical extensions and local grade variation of iron beds.

Field Study of Pirquitas mine in Jujuy Province, NW Argentina (아르헨티나 후후이주 삐르키타스광산의 현장조사 연구)

  • Lee, Han-Yeang
    • The Journal of the Petrological Society of Korea
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    • v.16 no.4
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    • pp.189-195
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    • 2007
  • Pirquitas mine was Bolivian type deposits, which Tertiary quartz andesites caused various epithermal quartz veins and deposited minerals of Sn and Ag in it. Main mineral was cassiterite and necessaries were pyrite, arsenopyrite, pynhotite, Probable ore reserve and daily production are 200 million tons and 5 thousand tons, respectively, and both of exploration and pit development are being carried simultaneously, but in near future open pit works can be done. This mine is owned by the Canadian company of "Silver Standard Resources" and it is located on $S22^{\circ}30'25.0",\;66^{\circ}15'22.5"$, 4086m S.L. In view of infrastructure, geological environment and scale of ore reserves it is high potential area for domestic mining companies to participate share ownership.