Rock magnetic and dielectric characterizations of a formational contact in cretaceous strata (eastern Venezuela)

Abstract

Rock magnetic and dielectric studies have been conducted in sedimentary rocks close to a lithological contact (Chimana and Querecual formations) at the Pertigalete sedimentary sequence (Cretaceous northeastern Venezuela). Rock magnetic results suggest that the presence of secondary magnetic minerals has been conditioned by the transitional zone between Chimana and Querecual. In fact, this contact might have acted as a conduit for fluid circulation and a focus of chemical alteration on most of its adjacent strata. Some of the secondary magnetic minerals (e.g. magnetite) must be the outcome of the anoxic conditions that prevailed during times when the sedimentary basin reached its maximum temperatures when oil and gas were generated (Lower Miocene). Some others (e.g. hematite) are the likely byproduct of alteration dating from times when oxidizing conditions were dominant. The Thermally Stimulated Depolarization Current (TSDC) technique is used here to dielectrically characterize the same contact. The complex TSDC spectra obtained in the temperature range from 77 to 230 K for the samples studied, indicate a notable difference between the Chimana (CH) and Querecual (QC) samples. Drying and rehydration treatments performed on these samples show that the whole depolarization spectrum is mainly due to moisture trapped in the microporosity of the material. The broad spectra, separated by using Direct Signal Analysis, reveal the presence of four overlapping peaks. TSDC results indicate a progressive change in the mean re-orientation energy with the lithology for the four relaxations. This variation, due to the change in the environment seen by the water dipoles hydrogen-bonded to different sites in the material, is observed for the same lithologies where magnetic anomalies have been reported. Thus, rock magnetic analyses, combined with the TSDC technique, seem to serve as a sensitive and alternative means of characterizing lithologies and stratigraphic discontinuities in a sedimentary sequence.