<p>SECTION 1: Introduction<br>1. Tectonic inheritance and structural styles in the Andean fold-thrust belt and foreland basin <br>2. Seismic imaging in fold-and-thrust belts<br>3. Analogue modeling as a tool to assist seismic structural interpretation in the Andean fold-and-thrust belt </p> <p>Section 2: Field analog<br>4. Folding of a weak boundary zone between an axial and a frontal belt, Chicamocha Valley, Eastern Cordillera of Colombia<br>5. Natural examples of regional-scale structures from the southern Central Andes and Patagonian Andes<br>6. Outcrop-scale natural examples of structures from the southern Central Andes</p> <p>SECTION 3: Colombia<br>7. Thrust sequence in the Sinu Fold Belt (South Caribbean Deformed Belt), offshore northwest Colombia<br>8. Relationships between normal faulting, mud diapirism and thrusting in the trailing part of the Sinú Fold Belt (South Caribbean Deformed Belt), offshore northwestern Colombia<br>9. Strike-slip fault zone in an oblique convergent margin. Bahia Basin Caribbean margin of Northern Colombia<br>10. Structural styles of the Upper Magdalena Valley, Northern Andes, Colombia: case studies<br>11. Forelimb deformation in basement uplifts. Examples from the Sierra de la Macarena, Colombia<br>12. Seismic expression of structural styles of transpressional thick skin deformation in the southern foothills of Colombia.<br>13. Structural styles and evolution of the Colombian Eastern Foothills Piedemonte triangle zone<br>14. Seismic and structural analysis of the San Francisco oil field (Colombia). Structural controls on a complex hydrocarbon charge history<br>15. La Cira Basement-high; Middle Magdalena Valley Basin, Colombia<br>16. Regional Structure, Trap Mechanisms and Basin Evolution of the Middle Magdalena Basin of Colombia<br>17. Structural Styles of the Southern Putumayo Basin, Northern Andes, Colombia</p> <p>SECTION 4: Ecuador<br>18. An appraisal of basin development at the trailing edge of the Northern Andes, SW Ecuador – NW Peru<br>19. The Manabí and Esmeraldas-Borbón forearc basins of Ecuador</p> <p>SECTION 5: Peru<br>20. Situche Complex, Marañon Basin. Peru<br>21. Large transport thrust in the Huallaga Basin (Northern Peruvian Sub-Andean Zone)<br>22. The San Martín anticline: a classic example of a fault-bend fold in the Camisea fold and thrust belt, Central Andes, Perú<br>23. The Sagari-Kinteroni Anticline: An Example of an Out-of-Sequence Tectonic Wedge in the Camisea Area, Peru<br>24. The Candamo antiformal stack, Madre de Dios Basin, Peru</p> <p>SECTION 6: Bolivia<br>25. Fault-related fold evolution in the Northern Sub-Andean of Bolivia<br>26. Transition from thin- to thick-skinned tectonics: example from the Boomerang Hills, Bolivia<br>27. Structural interpretation in the bolivian southern subandean: from surface to prospect generation<br>28. Seismic Interpretation challenges in the southern subandean fold and thrust belt of Bolivia<br>29. Thin Skinned Fold Belt Structural Style in the Argentinean-Bolivian Subandean Foothills, the Madrejones Anticline Example</p> <p>SECTION 7: Argentina<br>30. Structural styles of the Villa Unión-San Isidro basement-involved fold and thrust belt, Northern Ischigualasto-Villa Unión Basin province of La Rioja, Argentina<br>31. Structural styles, tectonic evolution and petroleum systems of transverse pre-Andean structures: examples from the Cuyo and Neuquén basins<br>32. Structure beneath the southern Payenia volcanic field, Neuquén Basin, Argentina.<br>33. Structural development in the frontal Malargüe fold and thrust belt, Neuquén Basin, Argentina<br>34. Interpreting a complex Triangle Zone in the Agrio Fold Thrust Belt, Neuquén Basin. Argentina<br>35. Exploration in a thick to thin-skinned transition, Falla Plegada Triangle Zone, Neuquen, Argentina<br>36. Foothills structure of the Andes of Tierra del Fuego, Argentina and Chile</p> <p>SECTION 8: Chile<br>37. Inverted structures in the western Central Andes thrust belt front <br>38. Interaction between Inverted and basement-involved reverse faults in the inner forearc of the Central Andes: an example from the Salar de Atacama Basin</p>
