Gravity Studies at Cerro Machín Volcano, Colombia

Authors

  • Nicolas Universidad de los Andes, Bogotá, Colombia
  • Juan Diego Universidad de los Andes, Bogotá, Colombia
  • Indira Universidad de los Andes. Now at Servicio Geológico Colombiano, Bogotá, Colombia https://orcid.org/0000-0003-2300-1690
  • Andrés Universidad de los Andes, Bogotá, Colombia.

DOI:

https://doi.org/10.32685/0120-1425/bol.geol.49.1.2022.619

Additional Files

How to Cite

Pedraza, N. F., Velazquez, J. D., Molina, I., & Pedraza, A. (2022). Gravity Studies at Cerro Machín Volcano, Colombia. Boletín Geológico, 49(1), 55–65. https://doi.org/10.32685/0120-1425/bol.geol.49.1.2022.619

Issue

Section

Articles

Published

2022-06-30

Abstract

A gravimetric study was performed at the Cerro Machin volcano (4° 29’ N, 75° 22’ W), Tolima Department, Colombia,  to obtain a density distribution of the volcanic edifice and its basement. This study was divided into three main sections.  The first section consisted of gravimetric measurements on  the volcano, which were performed with a Scintrex Autograv CG-5 gravimeter. In the second section, a complete Bouguer anomaly was obtained by applying gravimetric corrections  to the field data, such as instrumental drift, latitude, free-air, Bouguer, and topographic corrections. For the third section, we used the GM-SYS extension of Oasis Montaj to obtain a forward model of the subsurface density distribution that  allowed us to explain the source of the gravimetric anomaly. As the main results for this study, we determined that the  field-obtained Bouguer anomaly ranged between -87 mGal and -29 mGal in the study area. The Oasis Montaj density  model allowed us to infer an elongated dacitic complex at  the top of the distribution with a mean density of 2300  kg/m3, with the presence of a volcanic conduit of 2400  kg/m3 at the base. The seismicity in the area suggests that  the gravimetric anomaly caused by the dome and its  surrounding materials may be related to a large weakened zone at the interface between the volcanic edifice and the  metamorphic basement, provoked by fault activity,  interaction with the hydrothermal system and the ascent of  hot, fluid material to the surface. This study suggests one  interpretation of the Machin dome volcanic complex and  encourages further gravimetric studies and modeling over a wider area. 

Author Biographies

Nicolas, Universidad de los Andes, Bogotá, Colombia

Geoscientist with an interest in working in geology and exploration geophysics. I have the ability to integrate the branches of geology, geophysics and the use of remote sensors for different studies in the earth sciences.

Juan Diego, Universidad de los Andes, Bogotá, Colombia

Geoscientist with special interest in the areas of Geophysics and Volcanology. I have basic knowledge of mineralogy, stratigraphy, petrology, seismic, seismology and structural geology, as well as the basic concepts of mineral and hydrocarbon exploration

Indira, Universidad de los Andes. Now at Servicio Geológico Colombiano, Bogotá, Colombia

Seismologist of the National Seismological Network of Colombiam with interest in the use of applied and fundamental research in solving geological problems, such as crustal models, modeling of seismic events, fluid migration, tectonic models and pre-eruptive phenomena.

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