PALYNOFACIES AND ORGANIC GEOCHEMISTRY OF LACUSTRINE SOURCE ROCKS: THE POTRERILLOS – CACHEUTA SOURCE ROCK SYSTEM IN THE TRIASSIC CUYO BASIN, WEST-CENTRAL ARGENTINA
Juan A. Pineda1,2*, Marcos Comerio1,2, Eduardo G. Ottone3, Joaquín Salduondo4, Gastón Otegui2 and Georgina Erra5
1 CONICET, YPF Tecnología S.A., Avenida Del Petróleo s/n-(Entre 129 y 143) Berisso, Buenos Aires 1925, Argentina.
2 YPF Tecnología S.A., Avenida Del Petróleo s/n-(Entre 129 y 143) Berisso, Buenos Aires 1925, Argentina.
3 CONICET-Universidad de Buenos Aires. Instituto de Estudios Andinos Don Pablo Groeber (IDEAN), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, C1428EHA, CABA, Argentina.
4 CETMIC- CONICET. Centro de Tecnología de Recursos Minerales y Cerámica. Centro Científico Tecnológico (CCT) La Plata, CONICET, Manuel B. Gonnet, Argentina.
5 CONICET. División Paleobotánica, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina.
* Corresponding author: email juan.a.pineda@ypftecnologia.com
This study presents an integrated investigation of the Upper Triassic Potrerillos – Cacheuta lacustrine source rock in the Cuyo Basin of western Argentina. Data came from palynofacies analyses, organic petrography, Rock-Eval pyrolysis and mineralogical studies based on X-ray diffraction analyses. An 80 m thick outcrop section was studied and is interpreted to represent the transition from shallow-lacustrine sediments influenced by fluvial discharges (uppermost Potrerillos Formation) to the deposits of a deep, permanent lake (Cacheuta Formation). Three palynofacies were defined. Palynofacies I is characterized by shallowing-upward cycles with abundant woody material, and was deposited under an oxic, disturbed water column. Palynofacies II and III occur in laminated shales rich in amorphous organic matter (AOM) and freshwater algal material (Botryococcus) respectively, which were deposited under oxygen-depleted conditions. In general, the detrital material present suggests an input derived from fluvial discharges; however, interbedded tuffs altered to analcime and smectite suggest the transformation of vitric material in pyroclastic ash under saline to alkaline water conditions. Kerogen Types II/III and III with high total organic carbon values indicate a moderate oil- and gas-prone source rock whose thermal maturity varies from immature to the early oil window (Tmax: 430-438 ºC; vitrinite reflectance: 0.59-0.67 % VRo; and thermal alteration index: 2-2+).
This study demonstrates the importance of palynofacies analyses for the interpretation of depositional changes and associated controls in lacustrine shale successions. When integrated with data from organic geochemistry, palynofacies analysis is an important tool in the evaluation of a source rock’s thermal maturity and hydrocarbon generation potential.
Key words: palynofacies, lacustrine source rock, Potrerillos Formation, Cacheuta Formation, organic petrography, hydrocarbon potential, Cuyo Basin, Triassic, Argentina.
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