Garzón Massif basement tectonics: Structural control on evolution of petroleum systems in upper Magdalena and Putumayo basins, Colombia. (December 2017)

• Record Type: Journal Article
• Authors: Saeid, E.; Bakioglu, K.B.; Kellogg, J.; Leier, A.; Martinez, J.A.; Guerrero, E.
• Is Part Of: Marine and petroleum geology. Volume 88(2017)
• Page Start: 381
• Page End: 401
• Publication Date: 2017-12
• Subjects: Andean foreland basin -- Garzón massif -- Basement tectonics -- Thin-skinned thrusting -- Putumayo basin -- Gravity -- Magnetics -- Topoyaco -- Heavy oil -- Biodegradation -- Monocline; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2017.08.035
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: The Garzón Massif, is an active Laramide style basement uplift flanked by the Upper Magdalena Valley (UMV) and the Putumayo Basin. In this paper we use new gravity, magnetic, well and seismic data for the first geophysical interpretation of the Garzón Massif. The Garzón/Algeciras fault has been previously interpreted as a right-lateral strike-slip fault. The new seismic, well, and gravity data demonstrates that the Garzón fault is also a low-angle (12–17°) Andean age fault thrusting PreCambrian basement 10–17 km northwestward over Miocene sediments of the UMV in a prospective footwall anticline. The new geophysical data as well as previous field mapping were used to produce the first gravity and magnetic maps and retrodeformable structural cross section of the northern Garzón Massif. The new model distinguishes for the first time distinct episodes of "thin-skinned" and "thick-skinned" deformation in the Garzón Massif. The model indicates approximately 43 km of Early to Middle Miocene shortening by "thin-skinned" imbricate thrusting contemporaneous with the uplift of the nearby southern Central Cordillera (∼9–16 Ma) and the main hydrocarbon expulsion event for the UMV and Putumayo Basin. This was followed by at least 22 km of Late Miocene (3–6 Ma) "thick-skinned" Andean shortening and 7 km of uplift on the symmetrical Garzón thrust and a SE-verging basement thrust fault zone. The Andean uplift interrupted and exposed the hydrocarbon migration pathways to the Putumayo Basin. 3-D volume fracture analysis was used for the first time in this paper together with the first seismic and well data published for the Topoyaco and Miraflor structures to test closure models for the Topoyaco foothills. Intense fracturing is observed in the Topoyaco basement monocline from the near-surface to depths of over 3.5 km. The high level of fracturing permitted freshwater flushing and oil biodegradation and hydrocarbon escape. In contrast, the Miraflor-1 well, located just southwest of the Topoyaco block, tested light gravity oil and is sealed from groundwater flushing and biodegradation by a backthrust. Graphical abstract: Image 1 Highlights: 1st balanced x-section of Garzón Massif from seismic, well, and potential field data. Distinct episodes of "thin-skinned" and "thick-skinned" deformation critical for petroleum system. Garzón thin-skinned thrusting (9–16 Ma) coincided with hydrocarbon expulsion. Garzón thick-skinned basement uplifts (3–6 Ma) interrupted migration pathways. Garzón/Algeciras f., previously mapped as strike-slip, thrusts granite 10–17 km, 12–17°.