Berlin: Springer, 2007. — 491 p.
What is the important geologic information recorded in Thrust Belts and Foreland Basins (TBFB) on the evolution of orogens? How do they transcript the coupled influence of deep and surficial geological processes? Is it still worth looking for hydrocarbons in foothills areas? These and other questions are addressed in the volume edited by Lacombe, Lavé, Roure and Vergés, which constitutes the Proceedings of the first meeting of the new ILP task force on "Sedimentary Basins", held in December 2005 at the Institut Français du Pétrole, on behalf of the Société Géologique de France and the Sociedad Geologica de España. This volumes spans a timely bridge between recent advances in the understanding of surface processes, field investigations, high resolution imagery, analogue-numerical modelling, and hydrocarbon exploration in TBFB. With 25 thematic papers including well-documented regional case studies, it provides a milestone publication as a new in-depth examination of TBFB.
Показано строение и закономерности развития складчато-надвиговых поясов горно-складчатых систем и континентальных окраин. Освещены теоретические вопросы формирования складчатых зон, приведены практические примеры на основе материалов сейсморазведочных работ, рассмотрены вопросы нефтегазоносности складчато-надвиговых поясов.Surficial and Deep Processes in Thrust BeltsCoupled Lithosphere-Surface Processes in Collision Context
On Some Geometric Prism Asymmetries
Exploration of Thrust Belts: Seismic Imaging and TrapsUnderstanding Seismic Propagation Through Triangle Zones
2D Depth Seismic Imaging in the Gaspe Belt, a Structurally Complex Fold Thrust Belt in the Northern Appalachians, Quebec, Canada
Exploration of Thrust Belts: Fluid Flow and Hydrocarbon SystemsFluid Systems in Foreland Fold-and-Thrust Belts: An Overview from the Southern Pyrenees
The Miocene Petroleum System of the Northern Apennines in the Central Po Plain (Italy)
Structural Modeling / RestorationFolds Kinematics in “Fold and Thrust Belts”. The “Hinge Migration” Question, a Review
The Use of Surface Restoration in Foothills Exploration: Theory and Application to the Sub-Andean Zone of Bolivia
Plate Tectonic Setting and Cenozoic Deformation of Trinidad: Foldbelt Restoration in a Region of Significant Strike-Slip
Kinematics of the SE Canadian Foreland Fold-and-Thrust Belt: Implications for the Thermal and Organic Maturation History
Zagros/Makran Thrust BeltsEarly Reactivation of Basement Faults in Central Zagros (SW Iran): Evidence from Pre-Folding Fracture Patterns in Asmari Formation and Lower Tertiary Paleogeography
Evolution of Maturity in Northern Fars and Izeh Zone (Iranian Zagros) and Link with Hydrocarbon Prospectivity
Mechanical Constraints on the Development of The Zagros Folded Belt (Fars)
Rates and Processes of Active Folding Evidenced by Pleistocene Terraces at the Central Zagros Front (Iran)
The Salt Diapirs of the Eastern Fars Province (Zagros, Iran): A Brief Outline of Their Past and Present
The Role of Pre-Existing Diapirs in Fold and Thrust Belt Development
Impact of Sedimentation on Convergent Margin Tectonics: Example of the Makran Accretionary Prism (Pakistan)
Offshore Frontal Part of the Makran Accretionary Prism: The Chamak Survey (Pakistan)
Carpathian Thrust BeltThe Geometry of the Southleading Carpathian Thrust Line and the Moesia Boundary: The Role of Inherited Structures in Establishing a Transcurrent Contact on the Concave Side of the Carpathians
Role of the Foredeep Evaporites in Wedge Tectonics and Formation of Triangle Zones: Comparison of the Carpathian and Pyrenean Thrust Fronts
Reservoir Properties of Miocene Sandstones in Rzeszow Area (Carpathian Foredeep, Poland)
Relationship between Hydrocarbon Generation and Reservoir Developmentin the Carpathian Foreland (Poland)
Tectonics, Sedimentation and Denudation in Thrust BeltsTectonic and Climatic Controls on Sedimentation in Late Miocene Cortemaggiore Wedge-Top Basin (Northwestern Appennines, Italy)
Meso-Cenozoic Evolution of Mountain Range - Intramontane Basin Systems in the Southern Siberian Altai Mountains by Apatite Fission-Track Thermochronology
Slab Retreat and Active Shortening Along the Central-Northern Apennines