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Sedimentology and architecture of early post-rift submarine lobe deposits; the Los MoUes Formation, Neuquén Basin, Argentina

Author(s): Aurélia Privat Stratigraphy Group, School of Earth and Environment, University of Leeds, Leeds LS29JT, United Kingdom
David M. Hodgson Stratigraphy Group, School of Earth and Environment, University of Leeds, Leeds LS29JT, United Kingdom
Christoher A.-L. Jackson Department ofEarth Science & Engineering, Imperial College, Prince Consort Road, London, SW7 2BP, United Kingdom
Ernesto Schwarz Centro de Investigaçiones Geológicas (CIG), La Plata, Provincia de Buenos Aires, Argentina
Jeffrey Peakall Stratigraphy Group, School of Earth and Environment, University of Leeds, Leeds LS29JT, United Kingdom

The sedimentary architecture of submarine lobe-dominated successions in early post-rift settings are poorly understood despite commonly being proven hydrocarbon reservoir systems, in pmt because these types of systems are rarely exposed. Exhumed early post-rift deposits in the Neuquen Basin, Argentina, have been investigated in the Jurassic Los Molles Formation, to help understand and predict the subseismic dish·ibution of facies around inherited syn-rift structures. Two distinct depocenters, La Jardinera and Come Yeguas, are located between NW-SE trending extensional syn- rift footwall highs.

The well exposed submarine lobe-dominated successions have allowed sedimentological mad architectural changes in the Los Molles Formation to be constrained by use of coJTelation panels consh·ucted along a 12 km strike section in La Jardinera and a 2.5 km cross strike section towards syn- rift faults in Come Yeguas. The early post-rift deep-water stratigraphy is characterized by the onlap and pinchout of sandbodies, which in combination with hardground development on footwall highs indicates that deposition occurred across fault-block highs.

The basin physiography during deep-water deposition was, therefore, demonstrable conditioned by inherited syn-rift structures that influenced the timing and location of bypass, erosion and deposition of sand-rich sediment gravity flows. The infill architecture of the two depocenters record different stratigraphic architectures and stratal pattems of sand-rich strata, infeJTed to be the result ofthe conh·asting responses of marine clastic sedimentation to the inherited syn-rift topography, differential subsidence, sea-level variations mad sediment supply. This study provides criteria to decipher relationships between the organization of lobe deposits and inherited syn-rift structures that can be integrated to improve the prediction of reservoir bodies in underexplored early post-rift successions.


Title:
Sedimentology and architecture of early post-rift submarine lobe deposits; the Los MoUes Formation, Neuquén Basin, Argentina
Type:
Poster (Student)
Origin:
Academia
Day:
1
Session:
0
Daily sequence no.:
01
Lead author last name:
Privat
Lead author first name:
Aurélia
Affiliation(s):
Stratigraphy Group, School of Earth and Environment, University of Leeds, Leeds LS29JT
Country:
United Kingdom
Abstract status:
ok
UID:
86