Neogene-Quaternary seismic stratigraphy of the Llancanelo Lake Basin, Mendoza, Argentina

摘要

A new shallow multichannel seismic survey was carried out in the Llancanelo Lake region (SouthernMendoza Province, Argentina), in order to complete and extend previously surveyed seismic sections. The new seismicdata allowed to double the already existing data. The obtained information was correlated with seismic and stratigraphicdata from the industry. In this way it was possible to depict the major Neogene-Quaternary sedimentary-volcanicsequences and the regional evolution of a tectonic-volcanic basin located in a key region at the eastern foot of the Andescordillera. This research is settled on early studies that comprised seismic works reaching depths of 600-700 m as wellas geoelectric and electromagnetic surveys reaching the uppermost 80-100 m of the sequences. The obtained resultsindicate the presence of three major sedimentary units separated by conspicuous seismic horizons SR1, SR2 and SR3,respectively considered as representing the late Mesozoic transition from marine to continental deposition, the beginningof the Cenozoic basaltic volcanism, and the change from dominantly sedimentary to dominantly volcanic processes atthe base of the Quaternary. The resulting stratigraphic scheme reveals increasing volcanic (basaltic layers) intercalationswith depth that accommodate to the geometry of the depocenter.