Evolving Stratigraphic Techniques and Interpretation III
Room Hall Marie Curie
Poster session is from 9:00 AM to 1:00 PM Co-Chairs: P. Imbert, K. Van der Zwan, and C. Ravenne
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| Booth #: P27, | D. Sánchez, Jr, M. Delgado, Sr, S. Angulo, Jr: Paleogeography of the Early-to-Middle Miocene in the Tácata Oilfield (Capaya and Carapita Formations), Eastern Venezuelan Basin, North of Anzoátegui and Monagas States |
| Booth #: P28, | N. Aguilera-Franco, M. A. Prado-Peña, C. Santiago-Gomez: Sedimentary Evolution of the Cenomanian to Coniacian in the Guerrero-Morelos Basin, Southern Mexico |
| Booth #: P29, | E. Albouy, J. M. Laigle, M. C. Cacas: Improved Techniques of Stratigraphic Modeling Controlled by Seismic Data : Application to the National Petroleum Reserve, Alaska |
| Booth #: P30, | P. Bassant, P. (. Harris: Modeling Reservoir Architecture of Isolated Carbonate Platforms |
| Booth #: P31, | H. Gamero, C. Zavala, C. Contreras: A Reinterpretation of the Misoa Facies Types: Implications of a New Depositional Model, Maracaibo Basin, Venezuela |
| Booth #: P32, | J. A. M. Kenter, P. (. Harris, G. D. Porta: Microbial Boundstone Slope Shedding—a Model for Carbonate Platform Growth |
| Booth #: P35, | C. Xu, T. Cronin, B. Steer, T. Mcginness, T. Pickens: Turbidite Facies Analysis Through Integration of Electrical Images with Openhole Logs, Mudlogs and Map Data, Red Oak Field, Oklahoma, U.S.A |
| Booth #: P36, | J. L. P. Moreira, E. T. C. Abdalla, A. Z. N. Barros, L. F. Rodrigues: Shelf-Slope-Basin Depositional Systems of the Santos Basin Eocene Stratigraphic Sequence (BRazil Deep Seds—Deep-Water Sedimentation in the Southeast Brazilian Margin Project) |
| Booth #: P37, | J. L. P. Moreira, S. F. Santos, R. S. F. D'Avila, C. V. Madeira: Shallow- and Deep-Marine Siliciclastic Depositional Systems of the Santos Basin: How to Recognize Them (BRazil Deep Seds—Deep-Water Sedimentation in the Southeast Brazilian Margin Project) |
| Booth #: P38, | T. Jiang, X. Xie, J. Ren: Lowstand Fans Formation and Their Hydrocarbon Accumulation Since Middle Miocene, Yinggehai and Qiongdongnan Basins1 |