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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
- Affiliation(s):
- Stratigraphy Group, School of Earth and Environment, University of Leeds, Leeds LS29JT
- Country:
- United Kingdom
- Abstract status:
- ok
- UID:
- 86