Genesis of manganese oxide mineralization in the boleo region and concepción peninsula, baja california sur: Constraints from Pb-Sr isotopes and REE geochemistry

Rafael Del Rio-Salas, Lucas Ochoa-Landín, Christopher J. Eastoe, Joaquin Ruiz, Diana Meza-Figueroa, Martín Valencia-Moreno, Hugo Zúñiga-Hernández, Luis Zúñiga-Hernández, Verónica Moreno-Rodríguez, Héctor Mendívil-Quijada

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Manganese oxide mineralization on the eastern coast of Baja California Sur is intimately related to the Neogene tectonic evolution of the Gulf of California. Manganese is closely associated with the Cu-Co-Zn mineralization of the Boleo district and nearby deposits of Santa Rosalía region and Concepción peninsula. Trace element and rare earth element geochemistry of the manganese oxides provides clear evidence of a hydrothermal origin and excludes the hydrogenous nature for these deposits. Lead isotope data suggest that metal sources for the manganese mineralization along the eastern coast Baja California Sur are mostly the Miocene Andesite of Sierra Santa Lucía volcanics and the Peninsular Ranges batholith rocks. The strontium isotope data indicate that the mineralizing fluids involved in the manganese mineralization from Boleo district resulted from the interaction of two end-members: (1) the Sierra Santa Lucía volcanic rocks and (2) the gypsum member of the Boleo Formation. The geological observations and the available isotope and geochronological data suggest a southward migration of the hydrothermal processes in response to the evolving tectonic context of the opening of the Gulf of California.

Original languageEnglish (US)
Pages (from-to)482-499
Number of pages18
JournalRevista Mexicana de Ciencias Geologicas
Volume30
Issue number3
StatePublished - Nov 27 2013

Fingerprint

manganese oxide
rare earth element
geochemistry
isotope
mineralization
manganese
strontium isotope
lead isotope
coast
batholith
tectonic evolution
andesite
gypsum
Neogene
volcanic rock
Miocene
trace element
tectonics
fluid
metal

Keywords

  • Baja california
  • Manganese oxide
  • Mexico
  • Mineralization
  • Pb-Sr isotopes
  • Rare earth elements

ASJC Scopus subject areas

  • Geology

Cite this

Del Rio-Salas, R., Ochoa-Landín, L., Eastoe, C. J., Ruiz, J., Meza-Figueroa, D., Valencia-Moreno, M., ... Mendívil-Quijada, H. (2013). Genesis of manganese oxide mineralization in the boleo region and concepción peninsula, baja california sur: Constraints from Pb-Sr isotopes and REE geochemistry. Revista Mexicana de Ciencias Geologicas, 30(3), 482-499.

Genesis of manganese oxide mineralization in the boleo region and concepción peninsula, baja california sur : Constraints from Pb-Sr isotopes and REE geochemistry. / Del Rio-Salas, Rafael; Ochoa-Landín, Lucas; Eastoe, Christopher J.; Ruiz, Joaquin; Meza-Figueroa, Diana; Valencia-Moreno, Martín; Zúñiga-Hernández, Hugo; Zúñiga-Hernández, Luis; Moreno-Rodríguez, Verónica; Mendívil-Quijada, Héctor.

In: Revista Mexicana de Ciencias Geologicas, Vol. 30, No. 3, 27.11.2013, p. 482-499.

Research output: Contribution to journalArticle

Del Rio-Salas, R, Ochoa-Landín, L, Eastoe, CJ, Ruiz, J, Meza-Figueroa, D, Valencia-Moreno, M, Zúñiga-Hernández, H, Zúñiga-Hernández, L, Moreno-Rodríguez, V & Mendívil-Quijada, H 2013, 'Genesis of manganese oxide mineralization in the boleo region and concepción peninsula, baja california sur: Constraints from Pb-Sr isotopes and REE geochemistry', Revista Mexicana de Ciencias Geologicas, vol. 30, no. 3, pp. 482-499.
Del Rio-Salas, Rafael ; Ochoa-Landín, Lucas ; Eastoe, Christopher J. ; Ruiz, Joaquin ; Meza-Figueroa, Diana ; Valencia-Moreno, Martín ; Zúñiga-Hernández, Hugo ; Zúñiga-Hernández, Luis ; Moreno-Rodríguez, Verónica ; Mendívil-Quijada, Héctor. / Genesis of manganese oxide mineralization in the boleo region and concepción peninsula, baja california sur : Constraints from Pb-Sr isotopes and REE geochemistry. In: Revista Mexicana de Ciencias Geologicas. 2013 ; Vol. 30, No. 3. pp. 482-499.
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abstract = "Manganese oxide mineralization on the eastern coast of Baja California Sur is intimately related to the Neogene tectonic evolution of the Gulf of California. Manganese is closely associated with the Cu-Co-Zn mineralization of the Boleo district and nearby deposits of Santa Rosal{\'i}a region and Concepci{\'o}n peninsula. Trace element and rare earth element geochemistry of the manganese oxides provides clear evidence of a hydrothermal origin and excludes the hydrogenous nature for these deposits. Lead isotope data suggest that metal sources for the manganese mineralization along the eastern coast Baja California Sur are mostly the Miocene Andesite of Sierra Santa Luc{\'i}a volcanics and the Peninsular Ranges batholith rocks. The strontium isotope data indicate that the mineralizing fluids involved in the manganese mineralization from Boleo district resulted from the interaction of two end-members: (1) the Sierra Santa Luc{\'i}a volcanic rocks and (2) the gypsum member of the Boleo Formation. The geological observations and the available isotope and geochronological data suggest a southward migration of the hydrothermal processes in response to the evolving tectonic context of the opening of the Gulf of California.",
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