Bibliographies thématiques / Upper Valdarno Basin / Articles de revues

Articles de revues sur le sujet « Upper Valdarno Basin »

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Auteur : Grafiati
Publié le 10 mars 2023
Mis à jour le 11 mars 2023

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1

Ghinassi, Massimiliano. « Depositional environments of the Plio-Pleistocene Upper Valdarno Basin (Tuscany, Italy) ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 33–53. http://dx.doi.org/10.3301/ijg.2012.07.

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2

Fidolini, Francesco. « The Plio-Pleistocene fluvio-lacustrine Upper Valdarno Basin (central Italy) : stratigraphy and Basin fill evolution ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 13–32. http://dx.doi.org/10.3301/ijg.2012.06.

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3

Brogi, Andrea, Fidolini, Francesco et Liotta, Domenico. « Tectonic and sedimentary evolution of the Upper Valdarno Basin : new insights from the lacustrine S. Barbara Basin ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 81–97. http://dx.doi.org/10.3301/ijg.2012.08.

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4

Ielpi, A. « Sequence stratigraphy of a late Pliocene lignite seam (Upper Valdarno Basin, Northern Apennines, Italy) ». Rendiconti Online della Società Geologica Italiana, Volume 17 (1 novembre 2011) : 115–20. http://dx.doi.org/10.3301/rol.2011.36.

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5

Ghinassi, Massimiliano, et Alessandro Ielpi. « Morphodynamics and facies architecture of streamflow-dominated, sand-rich alluvial fans, Pleistocene Upper Valdarno Basin, Italy ». Geological Society, London, Special Publications 440, no 1 (10 février 2016) : 175–200. http://dx.doi.org/10.1144/sp440.1.

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6

Secci, M. Mori. « Palynological investigations on Pliocenic lacustre sediments in the «Castelnuovo dei Sabbioni» basin (upper Valdarno, central Italy) ». Webbia 46, no 2 (janvier 1992) : 265–75. http://dx.doi.org/10.1080/00837792.1992.10670524.

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7

Fidolini, Francesco, et Massimiliano Ghinassi. « Friction- and Inertia-Dominated Effluents In A Lacustrine, River-Dominated Deltaic Succession (Pliocene Upper Valdarno Basin, Italy) ». Journal of Sedimentary Research 86, no 9 (septembre 2016) : 1083–101. http://dx.doi.org/10.2110/jsr.2016.65.

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8

Rook, Lorenzo et Angelone, Chiara. « Just a few : rodents and lagomorphs in the Plio-Pleistocene fossil record of the Upper Valdarno Basin ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 98–103. http://dx.doi.org/10.3301/ijg.2012.27.

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9

Ghinassi, Massimiliano et Sagri, Mario. « Going over 30 years of geological and paleontological studies on the Pliocene-Pleistocene Upper Valdarno Basin (Tuscany, Italy) ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 5–12. http://dx.doi.org/10.3301/ijg.2012.39.

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10

Ielpi, Alessandro. « Orbitally-driven climate forcing in late Pliocene lacustrine siderite-rich clastic rhythms (Upper Valdarno Basin, Northern Apennines, Italy) ». Palaeogeography, Palaeoclimatology, Palaeoecology 331-332 (mai 2012) : 119–35. http://dx.doi.org/10.1016/j.palaeo.2012.03.004.

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11

Fidolini, Francesco et Andreetta, Anna. « Integrating sedimentological and palaeopedological data for palaeoenvironmental reconstruction : examples from the Plio-Pleistocene Upper Valdarno Basin (Northern Apennines, Italy) ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 149–66. http://dx.doi.org/10.3301/ijg.2012.26.

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12

Esu, Daniela et Ghinassi, Massimiliano. « The non-marine molluscs of the Plio-Pleistocene Upper Valdarno Basin (Tuscany, central Italy) : depositional environments, palaeoecology and biochronology ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 126–36. http://dx.doi.org/10.3301/ijg.2012.22.

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13

Bianchini, Silvia, Lorenzo Solari et Sandro Moretti. « Inventory and analysis of geological and topographic distribution of "Balze" crags in the Upper Valdarno basin (Tuscany region, Italy) ». Zeitschrift für Geomorphologie 60, no 4 (1 décembre 2016) : 311–26. http://dx.doi.org/10.1127/zfg/2016/0400.

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In this work we provide an analysis and an updated inventory map of the main outcropping crags, known as Balze in Italy, in the Upper Valdarno basin (Tuscany, Italy). These erosional forms develop in the alluvial-fan deposits that characterize this area. The study area extends up to 30 km2 within the local ANPIL (Natural Protected Area of Local Interest) and can be ascribed as a geomorphosite. Detection and mapping of Balze exposures were outlined on a pre-existing broad raster database, and then improved by means of photo-interpretation of optical imagery and analysis of Digital Terrain Model (DTM) and of topographic layers at 1:2,000 and 1:10,000 scale, supported by field work. A total of 151 Balze exposures were mapped and classified according to their progressive erosional stages, i.e.linear or indented escarpments, spire rocks and pinnacles or residual pillars. Furthermore, the spatial distribution of Balze scarps was investigated with respect to the geological and geomorphological setting and to the landscape zonation of the study area. Results of the inventory and analysis of geological and topographic distribution of the Balze crags can be useful for the characterization of the geomorphosite in the framework of its activity and management.
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14

Bertini, Adele, Maurizio Magi, Paul P. A. Mazza et Séverine Fauquette. « Impact of short-term climatic events on latest Pliocene land settings and communities in Central Italy (Upper Valdarno basin) ». Quaternary International 225, no 1 (septembre 2010) : 92–105. http://dx.doi.org/10.1016/j.quaint.2009.05.011.

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15

Bonini, Marco, Giovanna Moratti, Federico Sani et Maria Laura Balestrieri. « Compression-to-extension record in the Late Pliocene-Pleistocene Upper Valdarno Basin (Northern Apennines, Italy) : structural and thermochronological constraints ». Italian Journal of Geosciences 132, no 1 (février 2013) : 54–80. http://dx.doi.org/10.3301/ijg.2011.18.

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16

Zanetti, Florent, Thanh Thuy Nguyen Tu, Adele Bertini, Céline Egasse, Sylvie Derenne et Jean Broutin. « Chemotaxonomical investigations of fossil and extant beeches. II. Leaf lipids of Pliocene Fagus from the Upper Valdarno Basin, central Italy ». Comptes Rendus Palevol 6, no 6-7 (novembre 2007) : 515–25. http://dx.doi.org/10.1016/j.crpv.2007.09.003.

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17

Fidolini, Francesco, Massimiliano Ghinassi, Mauro Aldinucci, Paolo Billi, Jacopo Boaga, Rita Deiana et Lara Brivio. « Fault-sourced alluvial fans and their interaction with axial fluvial drainage : An example from the Plio-Pleistocene Upper Valdarno Basin (Tuscany, Italy) ». Sedimentary Geology 289 (mai 2013) : 19–39. http://dx.doi.org/10.1016/j.sedgeo.2013.02.004.

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18

BONINI, MARCO. « Basement-controlled Neogene polyphase cover thrusting and basin development along the Chianti Mountains ridge (Northern Apennines, Italy) ». Geological Magazine 136, no 2 (mars 1999) : 133–52. http://dx.doi.org/10.1017/s0016756899002277.

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The Chianti Mountains is an important sector of an E-verging regional thrust-related fold (the so-called Tuscan Nappe) extending along the whole length of the Northern Apennines. This thrust system involves the Tuscan Sequence superposing the Macigno sandstones onto Cervarola-Falterona sandstones, both of which are sedimented in adjacent foredeep basins. Detailed field mapping and analysis of superposition relations among tectonic structures, as well as correlation between structures and syntectonic deposition, has allowed Chianti Mountain evolution to be interpreted in terms of three main stages of deformation.The D1 stage resulted in the NE-directed synsedimentary thrusting of the Macigno onto the Cervarola-Falterona sandstones, while large NE to ENE-vergent thrust-related folds developed during the two successive deformation stages (D2 and D3). Fault-propagation folds developed during the D2 stage, and were affected by the Main Chianti Mountains Thrust (MCMT) during the successive D3 stage. In particular, the D3 stage has been correlated to the development, during the Pliocene period, of the hinterland Upper Valdarno Basin, which was previously considered to be an extensional basin. In fact, this continental basin formed along the eastern margin of the Chianti Mountains, ahead of the MCMT that also produced a shortening of the basin fill. With the beginning of the Quaternary period, the tectonic regime switched to extensional, as manifested by the development of a normal fault system on the opposite basin margin.The data presented here allow us to infer that the Chianti Mountains thrust system (D2 and D3) developed during a time interval spanning from the Late Miocene (∼12 Ma) until the Late Pliocene (∼2 Ma) periods. In the Northern Apennines, polyphase thrusting recorded by cover rocks has been related to the activity of basement thrusts, which have been recently evidenced by geophysical data. In this context, the two latest stages of deformation recognised in the Chianti Mountains have been attributed to the activity of the Abetone–Cetona crustal thrust, the deformational effects of which propagated forward in the sedimentary cover.
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19

Ielpi, Alessandro. « Anatomy of major coal successions : Facies analysis and sequence architecture of a brown coal-bearing valley fill to lacustrine tract (Upper Valdarno Basin, Northern Apennines, Italy) ». Sedimentary Geology 265-266 (juillet 2012) : 163–81. http://dx.doi.org/10.1016/j.sedgeo.2012.04.006.

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20

Bertini, Adele. « Climate and vegetation in the Upper Valdarno Basin (central Italy) as a response to Northern Hemisphere insolation forcing and regional tectonics in the late Pliocene-early Pleistocene ». Italian Journal of Geosciences, Vol. 132, N. 1 (19 février 2013) : 137–48. http://dx.doi.org/10.3301/ijg.2012.18.

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21

CIRILLI, OMAR. « <em>EQUUS STEHLINI</em> ; AZZAROLI, 1964 (PERISSODACTYLA, EQUIDAE). A REVISION OF THE MOST ENIGMATIC HORSE FROM THE EARLY PLEISTOCENE OF EUROPE, WITH NEW INSIGHTS ON THE EVOLUTIONARY HISTORY OF EUROPEAN MEDIUM- AND SMALL-SIZED HORSES ». RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA 128, no 1 (21 février 2022). http://dx.doi.org/10.54103/2039-4942/15744.

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The present work provides a revision of the complete fossil collection of Equus stehlini from the Italian Early Pleistocene (late Villafranchian) of the Upper Valdarno Basin (Tuscany, Italy). The species was originally described in the second half of the last century, even if recent studies questioned its distinct species status, considering it a subspecies of Equus senezensis (i.e., E. senezensis stehlini). Over the succeeding decades the debate about the taxonomic status of E. stehlini extended to its possible evolutionary origin from two different Equus species from the European Early Pleistocene, Equus stenonis or E. senezensis. The revision undertaken here of E. stehlini, by means of morphological, morphometric and statistical comparisons, provides new insights into the taxonomic status and the evolutionary history of this enigmatic species. It is concluded that E. stehlini is a distinct species derived from the medium-sized E. senezensis. This work further highlights new insights and perspectives in the evolutionary framework and in the paleoecological understanding of the medium to small-sized Equus species from the early to middle Early Pleistocene of Europe.
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