Aburrá's Valley Geology.

This article is based on the information contained in the bachelor's degree project of the geologist Andrés Acevedo Gómez. The full reference of the work is the following: A. Acevedo, D. A. Rendón et al., Construcción de un modelo interpretativo 3D hasta 30 Km de profundidad de la corteza alrededor del Valle de Aburra, BSc Thesis, EAFIT University, 2012.

It has been reproduced with permission of the authors.

Area of Study

The area of study comprehends Aburra's Valley and its surroundings, its limited at north and at the east by the head of the municipality of Barbosa and the flat coordinates y=1 205 000 and x=863 000 respectively, at the south by the flat coordinate y=1 645 000 and the head of the municipality of Caldas, and at west by the Western limit of the Quebradagrande formation. The coordinate system is Bogota 1975 / Colombia Bogota zone EPSG:21892.

To make this project, the cartography used in Rendón, D. A., 2003. Tectonic and sedimentary evolution of the Upper Aburrá Valley, northern Colombian Andes. Tesis de Maestría, Universidad de Shimane. Japón, 203 pp. Was used.

The base map geology is shown in the next map: (Using the options you can change which references you can see, like grids or position of the pointer)

The lithological units of the base map are, (without age order):

Unit name Unit color
Complejo Arquía
Complejo Ofiolítico
Complejo Polimetamórfico de la Cordillera Central
Complejo Quebradagrande
Cuerpos Plutónicos Cretácicos
Depósito de Vertiente
Diorita de Heliconia
Esquistos cuarzo-sericíticos y cloríticos
Gabros asociados al SFCR
Gneises sintectónicos
Migmatitas, granulitas y gneises anfibolíticos
Neis de la Iguaná
Rocas Ultramáficas
Secuencia Volcánica
Sedimentos Terciarios
Stock de Altavista
Stock de San Diego

Cross Sections.

Using the cartographical, geological and geophysical information, 21 cross sections, east west, with a separation of 2 Km and a depth of 30 Km were created. 11 of those sections can be found in [[article:Secciones Transversales]]. In the next interactive visualization in 3 dimensions, you can see these cross sections and the geological map: