
Evolution of the Pyrenees during the Variscan and Alpine Cycles, Volume 2
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Evolution of the Pyrenees during the Variscan and Alpine Cycles 2 then highlights the contributions of several innovative approaches used to better constrain the transition from compressive to post-compressive tectonics. These include studies of relief flattening and incision processes; U-Pb geochronology applied to fault-related carbonates; cosmogenic nuclide dating combined with geomorphological analyses; and investigations into the thermal evolution of the Pyrenean rift basins. The book also documents Quaternary glacial fluctuations that affected the Pyrenees.
In conclusion, it presents a geological map of the northern slope of the mountain range at a scale of 1:250,000 and draws attention to the uniqueness of Pyrenean blue corundum.
Nicolas Saspiturry is a teacher-researcher specializing in the tectonic- sedimentary and thermal evolution of sedimentary basins. He has devoted much of his work to the Pyrenees.
Jessica Uzel has a doctorate in geology and a degree in life, earth and universe sciences. She specializes in the post-compressive evolution of the Pyrenean domain.
Alexandre Ortiz has a doctorate in geology. He specializes in the syn- to post-compressive evolution of the North Pyrenean foreland basin.
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Nicolas Saspiturry is a teacher-researcher specializing in the tectonic- sedimentary and thermal evolution of sedimentary basins. He has devoted much of his work to the Pyrenees.
Jessica Uzel has a doctorate in geology and a degree in life, earth and universe sciences. She specializes in the post-compressive evolution of the Pyrenean domain.
Alexandre Ortiz has a doctorate in geology. He specializes in the syn- to post-compressive evolution of the North Pyrenean foreland basin.
Content
- Cover
- Title Page
- Copyright Page
- Contents
- Preface
- Chapter 1. Structure of the Pyrenees at the Crustal Scale
- 1.1. Introduction
- 1.2. Tectonic framework of the Pyrenean belt
- 1.3. Crustal investigations by deep seismic reflection surveys
- 1.3.1. Results of the ECORS profiles across the Pyrenees
- 1.3.2. Contributions by recent geophysical surveys
- 1.4. Significance of high-density bodies at crustal depths
- 1.5. Serial crustal sections for the Pyrenees
- 1.5.1. The ECORS-Pyrenees section
- 1.5.2. The Nestes-Cinca section
- 1.5.3. The Chaînons Béarnais-Jaca section
- 1.5.4. The Basque-Cantabrian Pyrenees section
- 1.5.5. The Eastern Pyrenees section
- 1.6. Models for the crustal structure previous to the Pyrenean orogeny
- 1.7. The nature of the rifted continental margins
- 1.8. Rift inheritance and orogeny
- 1.9. References
- Chapter 2. Syncompressive Alluvial Conglomerates: Markers of Exhumation in the Eastern Pyrenees
- 2.1. Introduction
- 2.2. Geological context
- 2.3. Study methodology
- 2.4. Conglomerates of the eastern Pyrenees
- 2.4.1. The North Pyrenean area of Puivert
- 2.4.2. The South Pyrenean sector of Sant Llorenç de Morunys
- 2.4.3. Interpretation
- 2.5. Discussion - clasts as markers of the exhumation of the Pyrenees
- 2.6. Conclusion
- 2.7. References
- Chapter 3. Tectono-Sedimentary Evolution of the Aquitaine Basin from the Priabonian to the Pliocene
- 3.1. Introduction
- 3.2. Definitions and keywords related to foreland basins
- 3.3. Synthesis of structural, sedimentary, paleogeographic and biostratigraphic data from the Aquitaine Basin
- 3.3.1. Main tectonic structures of the Aquitaine Basin
- 3.3.2. Deformation timelines
- 3.3.3. Paleogene sedimentary infill of the Aquitaine Basin
- 3.3.4. Biostratigraphic calibrations
- 3.4. Evolution of sedimentary infill from the Priabonian to the Pliocene
- 3.4.1. Paleogeography of the Late Priabonian (35.1-33.8 Ma)
- 3.4.2. The Oligocene period (33.9-23.03 Ma)
- 3.4.3. The period from the Aquitanian to the Burdigalian (23.03-15.97 Ma)
- 3.4.4. Paleogeography of the Langhian and Serravallian
- 3.4.5. Paleogeography of the Tortonian and Messinian
- 3.4.6. Paleogeography of the Pliocene
- 3.5. Summary of the post-Priabonian tectonic evolution of the Aquitaine Basin
- 3.5.1. The Oligocene, final phase of syn-orogenic structuring
- 3.5.2. The Aquitanian, the transition to a post-orogenic regime
- 3.5.3. From the Burdigalian to the Tortonian, the final major deformation phase in the Aquitaine Basin
- 3.6. Conclusion
- 3.7. References
- Chapter 4. The Source-to-Sink Evolution of the Jaca Basin (Southern Pyrenees)
- 4.1. Introduction and geological background
- 4.2. Chronostratigraphic framework of the Jaca basin
- 4.3. Source area domains during the evolution of the basin
- 4.3.1. Source rock bulk petrology
- 4.3.2. U-Pb zircon geochronology
- 4.3.3. Heavy mineral content
- 4.4. Provenance evolution of the Jaca basin
- 4.4.1. The Early to Middle Eocene basin: Hecho Group turbidites
- 4.4.2. The Middle Eocene to Early Miocene basin: from transitional to terrestrial environments
- 4.5. References
- Chapter 5. The Western Mediterranean Extension and the Dismantling of the Eastern Pyrenees
- 5.1. Introduction
- 5.2. Origin and timing of extensional deformation
- 5.3. The tectonic dismantling of the eastern Pyrenees mountain chain
- 5.4. References
- Chapter 6. A "Late Pyrenean" Phase at the Burdigalian/ Langhian Transition (Corbières, France)?
- 6.1. Introduction
- 6.2. The eastern north Pyrenean domain: the Corbières region
- 6.2.1. Geological context
- 6.2.2. Geodynamic timeline
- 6.3. Discovery of a new tectonic event at the Burdigalian/Langhian transition in the Corbières
- 6.3.1. U-Pb data
- 6.3.2. Structural data
- 6.4. A "Late Pyrenean" phase at the scale of the orogen?
- 6.5. Origins of the event
- 6.5.1. The Kabylies?
- 6.5.2. The Gulf of Lion?
- 6.5.3. A tectonic event on the scale of the European platform?
- 6.6. Conclusion
- 6.7. References
- Chapter 7. Planation Surfaces and Post-Compressive Evolution of the Pyrenean Chain
- 7.1. Geological context
- 7.1.1. Structural domains of the Pyrenees
- 7.1.2. Deep structure of the Pyrenees
- 7.1.3. Formation of the Pyrenean relief
- 7.1.4. Cenozoic climate history of the Pyrenees
- 7.2. Relict planation surfaces and weathering effects in the Pyrenees
- 7.2.1. High-elevation relict planation surfaces
- 7.2.2. Weathering and relict planation surfaces
- 7.3. Origin of the relics of Pyrenean planation surface(s)
- 7.3.1. Age of the relics of the highest planation surface
- 7.3.2. Models for the formation of the Pyrenean planation surfaces
- 7.4. Summary and discussion
- 7.5. References
- Chapter 8. Dating and Erosion Rates of the Pyrenees: In Situ-Produced Cosmogenic Isotopes
- 8.1. In situ-produced cosmogenic isotopes
- 8.1.1. History
- 8.1.2. The main in situ-produced cosmogenic isotopes used in Earth sciences
- 8.1.3. Differential equation governing the concentration of a cosmogenic isotope at the surface
- 8.2. Dating the exposure of a rock to cosmic rays
- 8.2.1. Dating glacial polished bedrock surfaces and moraines to establish the chronology of deglaciation
- 8.2.2. Dating of exposure of alluvial deposits
- 8.2.3. Uncertainty in exposure dating
- 8.3. Quantification of the denudation rate in the Pyrenees
- 8.3.1. Calculation of denudation rates from cosmogenic isotopes
- 8.3.2. Application in the Pyrenees
- 8.3.3. Uncertainty in denudation rates
- 8.4. Burial dating of a rock
- 8.4.1. Calculation of a burial age from a pair of cosmogenic isotopes
- 8.4.2. Application in the Pyrenees
- 8.4.3. Uncertainty on burial datings
- 8.5. Summary: cosmogenic isotopes in the Pyrenees
- 8.6. References
- Chapter 9. Post-Compressive Incision of the Pyrenean Valleys: Insights from Karst Records
- 9.1. How can we trace the post-compressive evolution of the Pyrenean chain?
- 9.2. Karst in the Pyrenees
- 9.2.1. Pyrenean karsts, witnesses of paleoenvironments since the Paleozoic
- 9.2.2. The eastern Têt valley and its relation with the Mediterranean domain
- 9.2.3. The upper Aude valley and its relation with the Sault plateau
- 9.2.4. The valleys of the Ariège and their large networks
- 9.2.5. The karsts of the central Pyrenees and the Basque country
- 9.3. How to record valley incision with karsts
- 9.3.1. Epiphreatic model and chronology of valley excavation
- 9.3.2. Karst: sediment trap and witness of landscape evolution
- 9.4. How to date sediments trapped in karst
- 9.4.1. Use of cosmogenic burial durations 26Al/10Be: a validated method for Plio-Quaternary evolution
- 9.4.2. Use of the 10Be-21Ne pair: a major analytical development for reconstructing the Miocene evolution of valleys
- 9.4.3. Relationship between cosmogenic burial durations and the position of the base level at a given instant
- 9.5. Main results from the study of karsts
- 9.5.1. Incision rates of the upper Têt valley since the Burdigalian
- 9.5.2. Aude valley: between tectonic influence and Mediterranean influence
- 9.5.3. Ariège valley: impact of tectonics and glaciations
- 9.5.4. The valleys of the central and western Pyrenees: a promising outline
- 9.6. Drivers of incision of the Pyrenean valleys from the Miocene to the present
- 9.6.1. The valleys of the eastern Pyrenees connected to the Mediterranean
- 9.6.2. The valleys of the western Pyrenees connected to the Atlantic and subject to glaciations
- 9.6.3. Lessons from the karsts
- 9.7. Conclusion and prospects
- 9.8. References
- Chapter 10. Evolution of the Geothermal Gradient from Cretaceous Rifting to Pyrenean Compression (Western Pyrenees)
- 10.1. Introduction
- 10.2. Tectono-sedimentary evolution of the Mauléon Basin from the Mesozoic to the Cenozoic
- 10.2.1. The Cretaceous rifting phase: formation of the hyper-extended Mauléon Basin
- 10.2.2. The Pyrenean compression phase: inversion of the Cretaceous rift basin and building of the orogenic prism
- 10.3. RSCM thermometry, an overview of the method and its use in the Pyrenees
- 10.3.1. Methodology and analysis tool
- 10.3.2. History of the application of the RSCM method in Pyrenees
- 10.4. The geothermal gradient: definition
- 10.4.1. The rifting context
- 10.4.2. The orogenic context
- 10.4.3. The erosional context
- 10.5. Mesozoic to Cenozoic evolution of the geothermal gradient of the Mauléon Basin: application of RSCM thermometry
- 10.5.1. Thermal peak age in the Mauléon Basin
- 10.5.2. Cretaceous paleogeothermal gradients estimated from RSCM thermometry
- 10.5.3. Distribution of the geothermal gradient from the proximal to distal domain of the Mauléon Basin during the Cretaceous
- 10.5.4. Evolution of the geothermal gradient during Pyrenean compression
- 10.6. Numerical thermal modeling of the Mauléon Basin
- 10.6.1. Opening of the Mauléon Basin
- 10.6.2. Stage of synorogenic sedimentation
- 10.6.3. Stage of continental collision and erosion
- 10.6.4. Postcollisional quiescence
- 10.7. References
- Chapter 11. Pleistocene and Holocene Glacial Fluctuations in the Pyrenees
- 11.1. Introduction
- 11.2. From the first cartographies to a relative chronostratigraphy of Pyrenean glacial margin deposits
- 11.2.1. A long sequence of moraine deposits into three sedimentary units
- 11.2.2. Confrontation between polyglacialists and monoglacialists (1950s-1960s)
- 11.2.3. Rehabilitation of polyglacialism and repositioning of the fronts contemporary with the maximum ice extent of the last glaciation
- 11.3. Radiocarbon dating contribution
- 11.3.1. Chronological model established on the north-facing slope
- 11.3.2. A chronological model confirmed on the southern slope?
- 11.4. Recent diversification of dating methods
- 11.4.1. The contribution of OSL ages
- 11.4.2. The contribution of in situ-produced cosmogenic isotopes
- 11.5. Conclusion
- 11.6. References
- Chapter 12. Digital Geological Map of the Northern Slope of the Pyrenees at 1:250,000 Scale
- 12.1. Construction of the digital geological map of the northern slope of the Pyrenees
- 12.1.1. Work of the RGF
- 12.1.2. Map legend, structures and contour smoothing
- 12.2. Presentation, organization and dissemination of the map data
- 12.2.1. Presentation of the main cartographic features of the Pyrenees
- 12.2.2. Organization of the data composing the digital map
- 12.3. Dissemination and availability of the digital geological map data at the 1:250,000 scale
- 12.4. References
- Chapter 13. The Corundums of the Albitites Related to the Urdach Lherzolites: Lapidary Enhancement
- 13.1. The magmatic albitites related to the lherzolites
- 13.1.1. Structural characteristics
- 13.1.2. Mineralogical characteristics
- 13.1.3. Geochemical characteristics
- 13.1.4. Genetic hypothesis for the Urdach albitites
- 13.1.5. Possible origin of corundum xenocrysts and polycrystalline inclusions in alkaline basaltic provinces
- 13.1.6. A unique example of emplacement related to the Pyrenean orogeny
- 13.2. Corundum
- 13.2.1. "Primary" corundum crystals
- 13.2.2. "Secondary" corundum crystals
- 13.3. The value of the "amateur" perspective in science
- 13.3.1. Field research and sample selection
- 13.3.2. Value of lapidary work prior to scientific analysis
- 13.4. References
- List of Authors
- Index
- EULA
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