Palynofacies and organic geochemical data of the Middle Jurassic Los Molles Formation, Neuquén Basin, Argentina: Depositional environments and hydrocarbon potential

MARTINEZ, M.A.; PRÁMPARO, M.B.; QUATTROCCHIO, M.E.; ZAVALA, C.A.

REVISTA GEOLóGICA DE CHILE

Servicio Nacional de Geologia y Mineria de Chile

Lugar: Santiago, CHILE; Año: 2008 p. 279 - 305

0716-0208

A multidisciplinary analysis of palynofacies in a sequence-stratigraphical framework, TOC (total organic carbon) and TAI (thermal alteration index) analysis, has been applied to outcrop samples of the uppermost Los Molles Formation (Middle Jurassic), Neuquén Basin, Argentina, in order to characterise the palaeoenvironmental and palaeoclimatic conditions during the deposition of this unit. Five types of palynofacies (P-1 to P-5) have been identified and are interpreted to indicate a restricted marine to inner neritic environment. In P-1 and P-4, a marine environment close to the terrestrial source area with moderate oxidizing conditions and energy, are suggested. In P-2, the assemblage of freshwater algae, acritarchs and prasinophytes suggest a marginal marine environment influenced by fluvial discharge. In P-3, the marine microplankton content reflects conditions ranging from a marginal-marine (sub-normal salinity) to an inner neritic environment. In P-5, a dysoxic marine environment (probably marginal) is suggested. Warm and relatively humid (abundance of Cheirolepidiaceae in association with Araucariaceae) and locally humid (presence of swamps or ponds, on the alluvial plains) conditions are inferred. TOC content (65% of the analyzed samples reach TOC values over 1%), TAI values (2 to 2+, transitional between an immature phase and the window of liquid petroleum generation) and kerogen type (P-1, P-2 and P-5 show transitional characteristics between kerogen type II and III, while P-3 and P-4 show characteristics of kerogen type III and occasionally type IV), suggest that in the studied area the Los Molles Formation has some hydrocarbon potential. However, kerogen state suggests that the anoxic-dysoxic  conditions of the site of deposition were not optimum for its preservation.