Start |Author Index | View Uploaded Presentations | Meeting Information

GSA Annual Meeting in Denver, Colorado, USA - 2016

Paper No. 275-7
Presentation Time: 9:35 AM

METALLIC MINERAL DEPOSITS OF CUBA: METALLOGENIC EPOCHS, DEPOSIT MODELS AND GEODYNAMIC ENVIRONMENT


NELSON, Carl1, PROENZA, Joaquín A.2, MELGAREJO, J.C.3, CAZAÑAS, Xiomara4, PÉREZ-VÁZQUEZ, R.G.5, AIGLSPERGER, Thomas6, TORRÓ, Lisard6 and GARCÍA-CASCO, Antonio7, (1)Consulting Geologist, Boulder, CO 80304, (2)Universitat de Barcelona, Departament de Mineralogia, Petrologia i Geologia Aplicada, Barcelona, Spain, (3)Universitat de Barcelona, Facultat de Geologia, Martí i Franquès s/n, Barcelona, 08028, Spain, (4)Instituto de Geología y Paleontología, La Habana, Cuba, (5)Instituto Superior Politécnico José Antonio Echeverría, La Habana, Cuba, (6)Universitat de Barcelona, Departament de Cristal.lografia, Mineralogia i Dipòsits Minerals, Barcelona, Spain, (7)Departamento de Mineralogía y Petrología, Universidad de Granada, Granada, Spain, carlericnelson@gmail.com

Cuba has a long mining history (including the oldest copper mine of the Americas) and hosts some of the world’s most important deposits of nickel, cobalt and chromium as well as significant resources of manganese, copper, gold, silver, zinc and iron. Six distinct metallogenic epochs are identified:

i) mid-Jurassic-Early Cretaceous: as the North and South American portions of Pangea drifted apart, sedimentary exhalative (Sedex) Cu-Zn-Pb deposits formed in rift-related sedimentary basins.

ii) Early Cretaceous (∼135-110 Ma): a primitive Caribbean volcanic arc (boninitic and IAT series) related to west-dipping subduction of Proto-Caribbean lithosphere produced ophiolitic chromite deposits, ultramafic-hosted Au-rich massive sulfide deposits as well as bimodal-mafic and mafic type volcanogenic massive sulfide (VMS) deposits. Ophiolites of Cuba host some of the world’s richest refractory-grade chromite deposits, especially in the Moa-Baracoa ophiolite massifs, including the largest ophiolitic chromite deposit of the Americas.

iii) Late Cretaceous (pre-75 Ma): maturation of the Caribbean arc (that evolved to calcalkaline and high-K calc-alkaline series) generated epithermal precious metal deposits, small porphyry copper deposits and Fe-Cu-Au skarn deposits.

iv) Latest Cretaceous (75 Ma)-Eocene. Collision of the Caribbean arc with the Maya block and Bahamas platform (tectonic emplacement of the volcanic arc and ophiolitic units onto the continental margin) produced orogenic gold deposits.

v) Paleocene (Thanetian) to Early-Middle Eocene: An immature volcanic arc in eastern Cuba (Sierra Maestra) erupted low-K island arc tholeiites that host Cu-Zn-Au VMS deposits and volcanogenic (Cuban type) manganese deposits. In addition, iron skarn deposits (IOCG “clan”) occur in volcanic rocks near a contact with calc-alkaline plutons of intermediate composition.

vi) Late Eocene to Quaternary: Uplift exposed ophiolitic peridotite massifs to intense tropical weathering. Ni-Co laterite deposits (with some of the largest reserves in the world) formed over the serpentinized peridotites, especially in eastern Cuba and near Camagüey.

Session No. 275

P4. Geologic Evolution of Cuba
Wednesday, 28 September 2016: 8:00 AM-12:00 PM
Mile High Ballroom 2A/3A (Colorado Convention Center)
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-277211
© Copyright 2016 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.
Back to: P4. Geologic Evolution of Cuba
<< Previous Abstract | Next Abstract >>