Patrones de Fracturamiento de los Frentes de Deformación del Piedemonte Llanero, Cordillera Oriental de Colombia

A. Beltrán; A.F. Rincón; J.A. Támara; R.O. López; A. Piraquive; A. Delvalle; A. Kammer

doi:10.3997/2214-4609-pdb.111.176

Patrones de Fracturamiento de los Frentes de Deformación del Piedemonte Llanero, Cordillera Oriental de Colombia
By A. Beltrán, A.F. Rincón, J.A. Támara, R.O. López, A. Piraquive, A. Delvalle and A. Kammer
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 9th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas, Sep 2006, cp-111-00126
DOI: https://doi.org/10.3997/2214-4609-pdb.111.176

Abstract

The Deformation Front of the Eastern Cordillera is defined on its eastern foothills<br>by an asymmetric anticline with steep forelimb (Farallones Anticline at Medina<br>Village) to overturned forelimb (Buenavista Anticline at Villavicencio City). These<br>structures may have transmited strains to the foreland.

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2006-09-24

2024-04-25

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Patrones de Fracturamiento de los Frentes de Deformación del Piedemonte Llanero, Cordillera Oriental de Colombia

Abstract

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Most Cited This Month Most Cited RSS feed

The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture