Relevant bibliographies by topics / Tertiary Piedmont Basin

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Academic literature on the topic 'Tertiary Piedmont Basin'

Author: Grafiati
Published: 9 March 2023
Last updated: 10 March 2023

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Journal articles on the topic "Tertiary Piedmont Basin"

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Natalicchio, Marcello, Francesco Dela Pierre, Pierangelo Clari, Daniel Birgel, Simona Cavagna, Luca Martire, and Jörn Peckmann. "Hydrocarbon seepage during the Messinian salinity crisis in the Tertiary Piedmont Basin (NW Italy)." Palaeogeography, Palaeoclimatology, Palaeoecology 390 (November 2013): 68–80. http://dx.doi.org/10.1016/j.palaeo.2012.11.015.

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Capponi, Giovanni, Laura Crispini, Laura Federico, Michele Piazza, and Barbara Fabbri. "Late Alpine tectonics in the Ligurian Alps: constraints from the Tertiary Piedmont Basin conglomerates." Geological Journal 44, no. 2 (March 2009): 211–24. http://dx.doi.org/10.1002/gj.1140.

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Festa, Andrea, and Giulia Codegone. "Geological map of the External Ligurian Units in western Monferrato (Tertiary Piedmont Basin, NW Italy)." Journal of Maps 9, no. 1 (January 9, 2013): 84–97. http://dx.doi.org/10.1080/17445647.2012.757711.

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Bonci, Maria Cristina, Davide Dagnino, Andrea Mandarino, Aaron Mazzini, and Michele Piazza. "Revision of Ostrea (Gigantostrea) gigantica Solander var. oligoplana Sacco and Ostrea (Ostrea) isseli Rovereto (Oligocene, Tertiary Piedmont Basin, NW Italy)." Carnets de géologie (Notebooks on geology) 21, no. 3 (February 24, 2021): 55–66. http://dx.doi.org/10.2110/carnets.2021.2103.

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The aim of this paper is the revision and redocumentation of Ostrea (Gigantostrea) gigantica Solander var. oligoplana Sacco, 1897, Ostrea (Ostrea) isseli n. denom. Rovereto, 1897, and Ostrea (Ostrea) isseli n. denom. var. elongata Rovereto, 1897. These taxa are from the Oligocene strata of the Molare Formation (Tertiary Piedmont Basin, southern Piedmont - central Liguria, NW Italy). The syntypes of O. (G.) gigantica var. oligoplana are in the "Collezione Bellardi e Sacco", at the Museo Regionale di Scienze Naturali di Torino; the syntypes of O. (O.) isseli and O. (O.) isseli var. elongata are in the "Collezione BTP" (BTP Collection, at the Dipartimento di Scienze della Terra, dell'Ambiente e della Vita - DISTAV - of the Università di Genova). The var. oligoplana is here moved to the species rank and allocated to the genus Pycnodonte Fischer von Waldheim, 1835. O. (O.) isseli and O. (O.) isseli var. elongata are recognized as junior synonyms of the Sacco's taxon. Rovereto (1897) compared his new species with Ostrea subgigantea Raulin & Delbos, 1855, a poorly known taxon, that is here figured for the first time and shown to represent a species different from P. oligoplana (Sacco, 1897).
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Martire, Luca, Marcello Natalicchio, Catalin Costel Petrea, Simona Cavagna, Pierangelo Clari, and Francesco Dela Pierre. "Petrographic evidence of the past occurrence of gas hydrates in the Tertiary Piedmont Basin (NW Italy)." Geo-Marine Letters 30, no. 3-4 (February 25, 2010): 461–76. http://dx.doi.org/10.1007/s00367-010-0189-8.

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Carrapa, B., and D. Garcia-Castellanos. "Western Alpine back-thrusting as subsidence mechanism in the Tertiary Piedmont Basin (Western Po Plain, NW Italy)." Tectonophysics 406, no. 3-4 (September 2005): 197–212. http://dx.doi.org/10.1016/j.tecto.2005.05.021.

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Lozar, Francesca, Pierangelo Clari, Francesco Dela Pierre, Marcello Natalicchio, Elisa Bernardi, Donata Violanti, Emanuele Costa, and Marco Giardino. "Virtual Tour of Past Environmental and Climate Change: the Messinian Succession of the Tertiary Piedmont Basin (Italy)." Geoheritage 7, no. 1 (February 8, 2014): 47–56. http://dx.doi.org/10.1007/s12371-014-0098-8.

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Maino, Matteo, Alessandro Decarlis, Fabrizio Felletti, and Silvio Seno. "Tectono-sedimentary evolution of the Tertiary Piedmont Basin (NW Italy) within the Oligo-Miocene central Mediterranean geodynamics." Tectonics 32, no. 3 (June 2013): 593–619. http://dx.doi.org/10.1002/tect.20047.

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Dela Pierre, Francesco, Elisa Bernardi, Simona Cavagna, Pierangelo Clari, Rocco Gennari, Andrea Irace, Francesca Lozar, et al. "The record of the Messinian salinity crisis in the Tertiary Piedmont Basin (NW Italy): The Alba section revisited." Palaeogeography, Palaeoclimatology, Palaeoecology 310, no. 3-4 (October 2011): 238–55. http://dx.doi.org/10.1016/j.palaeo.2011.07.017.

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Tropeano, Domenico. "High flow events and sediment transport in small streams in the ‘tertiary basin’ area in piedmont (Northwest Italy)." Earth Surface Processes and Landforms 16, no. 4 (June 1991): 323–39. http://dx.doi.org/10.1002/esp.3290160406.

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Dissertations / Theses on the topic "Tertiary Piedmont Basin"

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REGUZZI, SIMONE. "SEDIMENTOLOGY AND STRATIGRAPHY OF TURBIDITE SYSTEMS WITH CONTRASTING ARCHITECTURES: EXAMPLES FROM THE TERTIARY PIEDMONT BASIN (NW ITALY) AND THE TAZA-GUERCIF BASIN (NE MOROCCO)." Doctoral thesis, Università degli Studi di Milano, 2022. http://hdl.handle.net/2434/922848.

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Architectures of submarine fans and turbidite systems are endowed by a high grade of complexity, inherited by the large variability of depositional flows characterising them. This complexity is reflected upon the superimposition of depositional elements (e.g., channels, levées, splays, etc.) giving rise to contrasting sedimentary facies and geometries at different scales. Thus, the understanding and prediction of their heterogeneity over space is essential to obtain reliable depositional models, which can be applied in the field of natural resources exploration. Despite heterogeneities of facies and architectures in turbidite deposits are largely studied, several questions regarding evolutionary controls still remain open due to the intricate interplay between autocyclic and allocyclic factors and the lack of roboust chronostratigraphic (i.e., time-related) constraints to be applied to turbidite systems evolution. This doctoral work focuses on two turbidite units, different for facies, architectures, age, and depositional setting. The work pursues the goal of complementing sedimentological data (collected with cm-scale resolution) with bio-chronostratigraphic data (both novel and collected from the literature) in order to provide a trustworthy estimation of the geological time in turbidite systems depositional models. In the first two chapters an overview on sediment gravity flows and their evolutionary models is provided, emphasising classical facies and depositional geometries. In chapter three, the sedimentary architecture and the controls on the evolution of a channel-levée complex from the Tachrift Turbidite System (Upper Miocene, Melloulou Fm., TazaGuercif Basin, NE Morocco) is addressed. The studied complex is spectacularly well exposed and then suitable for detailed sedimentological logging with cm-scale resolution. Results show a tripartite stratigraphic organisation of the complex, including: (i) a lowermost mud-prone interval with relatively small (a few hundred of metres across and metre-thick) and vertically stacked channels fills, (ii) a middle interval (ca. 4 m-thick and >1 km-wide) made of dominantly amalgamated sandstones with eastward-directed lateral accretion packages (LAPs), and (iii) an uppermost interval made of vertically aggraded channel fills with variously directed LAPs and well-developed levées. This organisation suggests that, after a relatively short phase of inception (lowermost interval), the channel underwent a prolonged lateral migration, prior to become aggradational (uppermost interval). Proportions of turbidite vs. hemipelagic deposits suggest that the migrational and aggradational phases straddle a lapse of reduced turbidite input to the studied section of the slope. It is suggested that the observed architectural style turnaround reflects the feedback of channel morphodynamics, sediment input, and along-dip channel depth profile. In chapter four, the Rupelian Monastero Fm. turbidite system (Tertiary Piedmont Basin, NW Italy) is addressed. This 1100 m-thick turbidite system was deposited adjacent to a coeval and heteropic fan delta system (i.e., the Savignone Conglomerates), upon a south-eastward dipping clastic ramp, and consists of an apparently monotonous succession of thin-bedded sandstone-mudstone couplets intercalated by erosive-based amalgamated bedsets made of sandstones and conglomerates. The unit was studied along the best exposed and most continuous section (Val di Grue-San Gaudenzio section) by cm-scale resolution sedimentological logging. Thesedimentological data were subsequently complemented with bio-magnetostratigraphic data (novel and from the literature) to refine the depositional model. In addition, seismic lines interpretation (in professional partnership with Eni S.p.A.) was used to constrain the Monastero Fm. depositional setting in the host basin. Results provide information about facies and architecture of the Monastero Fm. and insights for analogue systems: (i) the investigated stratigraphy is dominated for the 60% of section thickness by a muddy heterolithic background (with a density of 3 beds/m on average) alternated with conglomeratic channel fills and sandy lobes, (ii) the 65% of the studied section is composed of sedimentary bed repetitions interpreted as hyperpycnites, (iii) these repetitions cohexist with ‘classical’ turbidite facies indicating that the latter may represent the transformation of the former, (iv) bio-magnetostratigraphic data suggest an average accumulation rate of 400 m/Ma for the Monastero Fm., with an estimated return period of sedimentary gravity flows lower than a few thousand years, (v) seismic interpretations confirm the confined nature of the Monastero Fm. turbidite system. In conclusion, the new results of this doctoral work suggest that the use of magneto-biochronology can provide useful constraints for depositional age models, thus contributing to enhance our understanding of the time-scale and control factors of changes in sediment delivery to deep-water.
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Zubieta-Rossetti, Jose David. "Les sédiments syn-orogéniques du subandin et de l'avant -pays de Bolivie." Phd thesis, 2001. http://tel.archives-ouvertes.fr/tel-00546038.

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Le bassin d'Avant-Pays Andin de Bolivie, situé à l'Est de la Cordillère des Andes, couvre une superficie de près de 500.000 km2 et présente une épaisseur de sédiments dépassant 6500 m dans sa partie proximale. L étude présentée se fonde sur l'analyse d'affleurements, de données de forages et de sismique 2D obtenus au cours de l'exploration pétrolière du bassin. Le remplissage du bassin provient essentiellement de l'érosion des formations paléozoïques et mésozoïques de la Cordillère Orientale. La structuration et l'intensité de la déformation de la chaîne se traduisent par un système de séquences grano et strato-croissantes qui caractérise la période Oligocène à Actuel. Les unités stratigraphiques caractérisent 5 périodes tectoniques: 10 Période Oligocène supérieur-Miocène inférieur: Formations Petaca, Areniscas Superiores-Transici6n, Naranjillos et Bala, cette dernière constituant un équivalent latéral septentrional de la Formation Petaca ; 2° Période Miocène moyen-supérieur: Formation Yecua ; 3° Période Miocène supérieur-Pliocène: Fonnations Tariquia et Quendeque; 4° Période Pliocène: Formations Guandacayet Charqui ; 5° Période Pliocène supérieur-Quaternaire : Formations Emborozu et Tutumo. La géométrie récente du bassin est contrôlée par la paléogéographie et par le bâti structural ancien dont les structures ont été réactivées durant les déformations tertiaires. La partie proximale du système constitue le Subandin et le Piedmont, cependant que la plaine Chaco-Beni représente la partie très faiblement déformée, voire non déformée, du bassin en direction de l'Est. Dans la partie centrale et distale du bassin, la zone du BoomerangChapare est contrôlée par un système de fractures transpressives subverticales. La succession Phanérozoïque et le socle Précambrien sont impliqués dans la déformation. Les effets de l'érosion et les discordances progressives de la série phanérozoïque sont bien caractérisés y compris dans la partie la plus proximale du bassin (Subandin et Piedmont). La génération, l'expulsion, la migration et le piégeage des hydrocarbures qui se sont effectués dans le bassin sont essentiellement liés aux événements tectono-sédimentaires des derniers 6 Ma. La génération des hydrocarbures a comporté au minimum deux étapes qui expliquent que différentes qualités et différentes origines d' hydrocarbures puissent être rencontrées dans une même structure; la première est liée à des roches-mères du Silurien-Dévonien inférieur et la seconde à des roches-mères du Dévonien moyen-supérieur.
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Book chapters on the topic "Tertiary Piedmont Basin"

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Smith, R. D. A. "Complex bedding geometries in proximal deposits of the Castelnuovo Member, Rocchetta Formation, Tertiary Piedmont Basin, NW Italy." In Atlas of Deep Water Environments, 244–49. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_36.

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Francesca, Lozar, Violanti Donata, Bernardi Elisa, Dela Pierre Francesco, and Natalicchio Marcello. "Calcareous Microfossils as Tracers of Major Palaeoceanographic Perturbations: The Case of the Onset of the Messinian Salinity Crisis in the Tertiary Piedmont Basin (Northwestern Italy)." In Springer Geology, 1123–27. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_215.

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Gnaccolini, Mario, Romano Gelati, Paolo Falletti, and Donata Catrullo. "Sequence Stratigraphy of the “Langhe” Oligo-Miocene Succession, Tertiary Piedmont Basin, Northern Italy." In Mesozoic and Cenozoic Sequence Stratigraphy of European Basins. SEPM Society for Sedimentary Geology, 1999. http://dx.doi.org/10.2110/pec.98.02.0233.

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Festa, Andrea. "Tectonic, sedimentary, and diapiric formation of the Messinian mélange: Tertiary Piedmont Basin (northwestern Italy)." In Mélanges: Processes of Formation and Societal Significance. Geological Society of America, 2011. http://dx.doi.org/10.1130/2011.2480(10).

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BARUFFINI, LUCA, CARLO CAVALLI, and LORENZO PAPANI. "Detailed Stratal Correlation and Stacking Patterns of the Gremiasco and Lower Castagnola Turbidite Systems, Tertiary Piedmont Basin, Northwestern Italy." In Submarine Fans and Turbidite Systems: Sequence Stratigraphy, Reservoir Architecture and Production Characteristics, Gulf of Mexico and International: 15th Annual, 9–21. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 1994. http://dx.doi.org/10.5724/gcs.94.15.0009.

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Carrapa, B., J. Wijbrans, and G. Bertotti. "Detecting provenance variations and cooling patterns within the western Alpine orogen through 40Ar/39Ar geochronology on detrital sediments: The Tertiary Piedmont Basin, northwest Italy." In Detrital thermochronology - Provenance analysis, exhumation, and landscape evolution of mountain belts. Geological Society of America, 2004. http://dx.doi.org/10.1130/0-8137-2378-7.67.

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Conference papers on the topic "Tertiary Piedmont Basin"

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Mosca, P., G. Bertotti, and J. Juez-Larré. "The Constraints to the Subsidence and Exhumation of Alpine Units and the Tertiary Piedmont Basin, NW Italy." In 70th EAGE Conference and Exhibition - Workshops and Fieldtrips. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609.20147922.

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Seman, Spencer Mark, and Andrew J. Smye. "ECLOGITE CLASTS OF THE TERTIARY PIEDMONT BASIN, LIGURIAN ALPS, ITALY: RB-SR GEO/THERMOCHRONOLOGIC CONSTRAINTS ON EXHUMATION RATES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306886.

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Journal articles
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