Articles
The Villamaría-Termales Monogenetic Volcanic Field, Central Cordillera, colombian Andes (Part II): Compositional characteristics
Pablo Osorio- Luis Alvaro Botero-Gómez
- Hugo Murcia
- Carlos Borrero
- Jeny Alejandra Grajales
Published 2018-09-25
Keywords
- Colombian Central Cordillera,
- volcanic field,
- monogenetic volcanism,
- subduction zones,
- lava domes
- adakitic-signature ...More
How to Cite
Osorio, P., Botero-Gómez, L. A., Murcia, H., Borrero, C., & Grajales, J. A. (2018). The Villamaría-Termales Monogenetic Volcanic Field, Central Cordillera, colombian Andes (Part II): Compositional characteristics. Boletín De Geología, 40(3), 103–123. https://doi.org/10.18273/revbol.v40n3-2018006
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Abstract
The Villamaría-Termales Monogenetic Volcanic Field (VTMVF) consists of at least 14 monogenetic volcanoes that are aligned along the Villamaria-Termales Fault System (VTFS; western flank of the Central Cordillera of Colombia). Petrography and geochemical data allowed to define the compositional features of this volcanic field. The petrographic analysis shows that: pyroxene + amphibole + plagioclase, is the common mineral association for all the volcanoes from the VTMVF. The presence of other mineral phases such as: olivine and quartz in some volcanoes established the only difference between the whole field. Geochemical data shows a great compositional variety in the VTMVF represented by the SiO2 content between ~56 and ~69 wt.%, and an adakitic signature represented by low Y content (10 - 19 ppm) and HREE values as well as high Sr content (>518 ppm). Comparing these characteristics with those from the polygenetic Nevado del Ruiz Volcanic Complex (NRVC), it is possible to suggest a genetic relationship between both and a likely common magmatic reservoir
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References
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doi: 10.18273/revbol.v40n1-2018003.
Bohórquez, O.P., Monsalve, M.L., Velandia, F., Gil, F., y Mora, H. (2005). Marco tectónico de la cadena volcánica más septentrional de la Cordillera Central de Colombia. Boletín de Geología, 27(44), 55-79.
Borrero, C., Toro, L.M., Alvarán, M., and Castillo, H. (2009). Geochemistry and tectonic controls of the effusive activity related with the ancestral Nevado Del Ruiz volcano, Colombia. Geofísica Internacional, 48(1), 149-169.
Borrero, C., Murcia, H., Agustín-Flores, J., Arboleda, M.T., and Giraldo, A.M. (2017). Pyroclastic deposits of San Diego maar, central Colombia: an example of a silicic magma-related monogenetic eruption in a hard substrate. In: K. Németh, G. Carrasco-Núñez, J.J. Aranda-Gómez, and I.E. Smith (ed.). Monogenetic Volcanism (pp. 361-374). London: Geological Society, Special Publications, 446.
Botero-Gómez, L.A., Osorio, P., Murcia, H., Borrero, C., y Grajales, J.A. (2018). Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte I): Características morfológicas y relaciones temporales. Boletín de Geología, 40(3), 85-102. doi: 10.18273/revbol.v40n3-2018005.
Bustamante, C., Cardona, A., Archanjo, C.J., Bayona, G., Lara, M., and Valencia, V. (2017). Geochemistry and isotopic signatures of Paleogene plutonic and detrital rocks of the Northern Andes of Colombia: A record of post-collisional arc magmatism. Lithos, 277, 199-209. doi: 10.1016/j.lithos.2016.11.025.
Cañón-Tapia, E. (2016). Reappraisal of the significance of volcanic fields. Journal of volcanology and Geothermal Research, 310, 26-38. doi: 10.1016/j.jvolgeores.2015.11.010.
Castillo, P.R. (2006). An overview of adakite petrogenesis. Chinese Science Bulletin, 51(3), 257- 268. doi: 10.1007/s11434-006-0257-7. Defant, M.J., and Drummond, M.S. (1990). Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347(6294), 662-665. doi: 10.1038/347662a0.
Gómez-Cruz, A., Sánchez, M., y Pardo-Trujillo, A. (1995). Edad y origen del “complejo metasedimentario Aranzazu-Manizales” en los alrededores de Manizales (departamento de Caldas, Colombia). Geología Colombiana, 19, 83-93.
Gómez, J., Montes, N.E., Novia, A., y Diederix, H. (2015). Mapa Geológico de Colombia. Escala, 1, 1000000. Servicio Geológico Colombiano.
González, H., y Londoño, A.C. (2002). Catálogo de las unidades litoestratigráficas de Colombia. Granodiorita de Manizales (K2E1gdm) Cordillera Central - Departamento de Caldas, 5 - 8.
González, L., y Jaramillo, C.M. (2002). Estudio neotectónico multidisciplinario aplicado a la Falla Villa María - Termales. Tesis, Facultad de Ciencias Exactas y Naturales, Programa de Geología, Universidad de Caldas, Manizales.
González-Garcia, J., and Jessell, M. (2016). A 3D geological model for the Ruiz-Tolima Volcanic Massif (Colombia): Assessment of geological uncertainty using a stochastic approach based on Bézier curve design. Tectonophysics, 687, 139-157. doi: 10.1016/j.tecto.2016.09.011.
Irvine, T.N., and Baragar, W.R.A. (1971). A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8(5), 523-548. doi: 10.1139/e71-055.
Irving, E. (1971). La evolución estructural de los Andes más septentrionales de Colombia. Boletín Geológico, 19(2), 1-90. INGEOMINAS.
Janoušek, V., Farrow, C.M., and Erban, V. (2006). Interpretation of whole-rock geochemical data in igneous geochemistry: introducing Geochemical Data Toolkit (GCDkit). Journal of Petrology, 47(6), 1255-1259. doi: 10.1093/petrology/egl013.
Jerram, D.A., and Martin, V.M. (2008). Understanding crystal populations and their significance through the magma plumbing system. In: C. Annen and G.F. Zellmer (ed.). Dynamics of Crustal Magma Transfer, Storage and Differentiation (pp. 133-148). Vol. 304. London: The Geological Society of London, Special Publications.
Kay, R.W. (1978). Aleutian magnesian andesites: melts from subducted Pacific Ocean crust. Journal of Volcanology and Geothermal Research, 4(1-2), 117-132. doi: 10.1016/0377-0273(78)90032-X.
Laeger, K., Halama, R., Hansteen, T., Savov, I.P., Murcia, H.F., Cortés, G.P., and Garbe-Schönberg, D. (2013). Crystallization conditions and petrogenesis of the lava dome from the ∼900 years BP eruption of Cerro Machín Volcano, Colombia. Journal of South American Earth Sciences, 48, 193-208. doi: 10.1016/j.jsames.2013.09.009.
Le Bas, M.J., Le Maitre, R.W., Streckeisen, A., and Zanettin, B. (1986). A chemical classification of volcanic rocks based on the total alkali-silica diagram. Journal of Petrology, 27(3), 745-750. doi: 10.1093/petrology/27.3.745.
Londoño, J.M. (2016). Evidence of recent deep magmatic activity at Cerro Bravo-Cerro Machín volcanic complex, central Colombia. Implications for future volcanic activity at Nevado del Ruiz, Cerro Machín and other volcanoes. Journal of Volcanology and Geothermal Research, 324, 156-168. doi: 10.1016/j.jvolgeores.2016.06.003.
Maloney, K.T., Clarke, G.L., Klepeis, K.A., and Quevedo, L. (2013). The Late Jurassic to present evolution of the Andean margin: Drivers and the geological record. Tectonics, 32(5), 1049-1065. doi: 10.1002/tect.20067.
Martin, H. (1986). Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas. Geology, 14(9), 753-756.
doi: 10.1130/0091-7613(1986)14<753:EOSAGG>2.0.CO;2.
Martin, H. (1999). Adakitic magmas: Modern analogues of Archaean granitoids. Lithos, 46(3), 411-429. doi: 10.1016/S0024-4937(98)00076-0.
Martínez, L., Valencia L., Ceballos, J., Narváez, B., Pulgarín, B., Correa, A., Navarro, S., Murcia, H., Zuluaga, I., Rueda, J., y Pardo, N. (2014). Geología y estratigrafía del Complejo Volcánico Nevado del Ruiz. Informe final, Bogotá – Manizales – Popayán. Servicio Geológico Colombiano. 853p.
Maya, M., y González, H. (1995). Unidades litodémicas en la Cordillera Central de Colombia. Boletín Geológico, 35(2-3), 43-57. INGEOMINAS.
McCourt, W.J. (1984). The geology of the Central Cordillera in the Department of Valle del Cauca, Quindío and NW Tolima. British Geological Survey, INGEOMINAS, Cali.
McCourt, W.J., Aspden, J.A., and Brook, M. (1984). New geological and geochronological data from the Colombian Andes: continental growth by multiple accretion. Journal of the Geological Society, 141, 831-845.
Mosquera, D. (1978). Geología del cuadrángulo K8 Manizales. Informe preliminar 1763. INGEOMINAS.
Murcia, H. (2015). Monogenetic volcanism in the western Arabian Peninsula: Insights from Late Quaternary eruptions in northern Harrat Rahat, Kingdom of Saudi Arabia. Ph.D. Thesis, The University of Auckland, Auckland, New Zealand.
Murcia, H., Borrero, C., and Németh, K. (in press). Overview and plumbing system implications of monogenetic volcanism in the northernmost Andes' volcanic province. Journal of Volcanology and Geothermal Research. doi: 10.1016/j.jvolgeores.2018.06.013.
Murcia, H., Lindsay, J.M., Németh, K., Smith, I.E.M., Cronin, S.J., Moufti, M.R.H., El-Masry, N.N., and Niedermann, S. (2016). Geology and geochemistry of Late Quaternary volcanism in northern Harrat Rahat, Kingdom of Saudi Arabia: implications for eruption dynamics, regional stratigraphy and magma evolution. In: K. Németh, G. Carrasco-Núñez, J.J. Aranda-Gómez, and I.E.M. Smith (ed.). Monogenetic Volcanism (pp. 173-204). Vol. 446. London: The Geological Society of London, Special Publications.
Németh, K. (2010). Monogenetic volcanic fields: Origin, sedimentary record, and relationship with polygenetic volcanism. In: E. Cañón-Tapia, and A. Szakács (ed.). What is a volcano? (pp. 43-66). Vol. 470. New York: Geological Society of America. doi: 10.1130/2010.2470(04).
Nivia, A., Marriner, G.F., Kerr, A.C., and Tarney, J. (2006). The Quebradagrande Complex: A Lower Cretaceous ensialic marginal basin in the Central Cordillera of the Colombian Andes. Journal of South American Earth Sciences, 21(4), 423-436. doi: 10.1016/j.jsames.2006.07.002.
Peccerillo, A., and Taylor, S.R. (1976). Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contributions to Mineralogy and Petrology, 58(1), 63-81. doi: 10.1007/BF00384745.
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