Peñasquito Polymetallic Mine
Geology
The country rock consists of Mesozoic sediments that were deposited in the Basin of Mexico (Mexico Geosyncline). These sediments were intruded by quartz-feldspar porphyries, quartz monzonite porphyries, and other feldspar-phyric intrusives in the late Eocene to the mid-Oligocene, which form sills, dikes, and stocks. The primary ore for the Peñasquito Polymetallic Mine is in two diatreme breccias, named the Peñasco and the Brecha Azul. The mineralization contains gold, silver, lead and zinc. The diatremes flare upward, and are filled with brecciated country rock and intrusions. The rock surrounding the diatremes contain disseminated galena, sphalerite and sulfosalts within phyllic (sericite–pyrite–quartz) and proplytic (chlorite–epidote–pyrite) hydrothermal alteration envelopes. Where the diatremes intersect limestone units manto deposits of ore mineralization occur.
2017 Protest
A week-long protest disrupted operations at the Peñasquito mine during the first week of October 2017. Goldcorp had been forced to "announce a temporary suspension of operations due to a blockade by truck drivers protesting a loss of contracts at the country’s biggest gold deposit."
References
- ^ Obel, Mike (15 December 2011). "10 Biggest Silver Mines in the World". International Business Times.
- ^ "Operations and Projects: Peñasquito". Newmont Goldcorp. Retrieved 2019-12-06.
- ^ Staff (2011). "Peñasquito Polymetallic Mine, Zacatecas, Mexico". Mining-technology.com of Net Resources International.
- ^ Belanger, Maryse; Pareja, Guillermo; Nahan, Peter (31 December 2010). "Peñasquito Polymetallic Operation, Zacatecas State, Mexico, NI 43-101 Technical Report" (PDF).
- ^ "Goldcorp says protesters end blockade at Peñasquito mine in Mexico". Reuters. 2017-10-08. Retrieved 2017-10-17.
24°39′18.27″N 101°41′49.455″W / 24.6550750°N 101.69707083°W