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230515 ||| eng |
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|a 9783036522524
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|a books978-3-0365-2252-4
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|a 9783036522517
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|a Liotta, Domenico
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|a The Apennines: Tectonics, Sedimentation, and Magmatism from the Palaeozoic to the Present
|h Elektronische Ressource
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| 260 |
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|a Basel
|b MDPI - Multidisciplinary Digital Publishing Institute
|c 2023
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| 300 |
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|a 1 electronic resource (454 p.)
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| 653 |
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|a seismic reflection profiles
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|a Umbria pre-Apennines
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|a mélange
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|a Elba Island
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|a non-rigid plate kinematics
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|a fold-and-thrust belt
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|a magmatism
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|a Gavorrano pluton
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|a out-of-sequence thrust
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|a serpentinite
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|a accretionary wedge
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|a pelagic deposits
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|a tectonics
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|a foreland basin systems evolution
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|a contact metamorphism
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|a passive margin inversion
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|a southern Tuscany
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|a nannoplankton
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|a sedimentation
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|a satellite geodesy
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|a earthquakes
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|a inner northwest Apennines
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|a current deformation
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|a burial and tectonic history
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|a active faults
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|a outer Marche Apennines
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|a palynomorphs
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|a quartzo-feldspathic rocks
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|a Miocene
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|a backthrust
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|a Apennines
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|a electrical resistivity tomography
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|a magnetostratigraphy
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|a tectonic window
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|a incised valley
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|a Southern Tuscany
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|a karst
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|a Tyrrhenian-Apennine system
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|a geochronology
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|a stylolites
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|a biostratigraphy
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| 653 |
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|a Research & information: general / bicssc
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| 653 |
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|a fluid flow
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| 653 |
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|a tectonic inversion
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|a fractures
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|a Plio-Quaternary evolution
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|a Corchia Cave
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|a Agri Valley
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|a fluvial sedimentology
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|a cretaceous
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|a Risanguigno Formation
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|a biostratigraphic constraints to foredeep deposition
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|a Tuscan Palaeozoic
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|a Carboniferous
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|a southern Apennines
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| 653 |
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|a extensional tectonics
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| 653 |
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|a Western Alps
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|a clumped isotope thermometry
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|a thrust sheets
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|a Coastal Structure
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|a liguride units
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|a Albidona Formation
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|a Alpi Apuane
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|a paleopiezometry
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|a shear zone
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|a Central Apennines
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|a palynology
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|a northern Apennines
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|a seep-carbonates
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| 653 |
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|a Monticiano-Roccastrada Unit
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| 653 |
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|a cold seepage
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|a strain partitioning
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| 653 |
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|a exhumation
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| 653 |
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|a wedge-top basin
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| 653 |
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|a extensional and contractional deformation
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| 653 |
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|a Earth sciences, geography, environment, planning / bicssc
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| 653 |
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|a palaeodrainage
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| 653 |
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|a rotation models
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| 653 |
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|a timing of contractional tectonics
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| 700 |
1 |
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|a Molli, Giancarlo
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| 700 |
1 |
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|a Cipriani, Angelo
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| 700 |
1 |
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|a Liotta, Domenico
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| 041 |
0 |
7 |
|a eng
|2 ISO 639-2
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| 989 |
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|b DOAB
|a Directory of Open Access Books
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| 500 |
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|a Creative Commons (cc), https://creativecommons.org/licenses/by/4.0/
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| 028 |
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|a 10.3390/books978-3-0365-2252-4
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| 856 |
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|u https://www.mdpi.com/books/pdfview/book/6998
|7 0
|x Verlag
|3 Volltext
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| 856 |
4 |
2 |
|u https://directory.doabooks.org/handle/20.500.12854/98945
|z DOAB: description of the publication
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|a 900
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|a 363
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|a 000
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|a 576
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|a 700
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|a The Apennine orogenic system is a natural laboratory for multidisciplinary and integrated studies. The evolution of the Apennines is framed by the fragmentation of Pangea and the development of the Tyrrhenian Basin. Thus, the Apennines have carried this memory from the Permian and Triassic-Early Jurassic rifting, to the Oligocene-Miocene collision, and finally to the Miocene-Present, during which extension and compression have progressively migrated eastwards. Magmatism, hydrothermalism, and sedimentation in the Apennines have accordingly evolved in time and space. In this Special Issue, multidisciplinary and integrated studies have been published improving our knowledge of the Apennines and discussing: (a) the development of deformation and metamorphism in different tectonic environments, from the rifting stage to the subduction, exhumation, and late-orogenic stages; (b) the Meso-Cenozoic tectono-stratigraphic evolution of sedimentary basins, and their role in the Apennine orogeny; (c) the thermochronological evolution of sedimentary units and the dating of deformation episodes through geochemical techniques; (d) the magmatism and its connection to geodynamic evolution, from the mountain chain to the Tyrrhenian Basin; (e) recent tectonics, as reconstructed through seismological and paleo-seismological studies; and (f) the crustal structure, as derived by geophysical methods and their interpretation.
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