Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Mauro Aldinucci"'
Autor:
Massimiliano Ghinassi, Mauro Aldinucci, Valeria Bianchi, Andrea Brogi, Enrico Capezzuoli, Tsai-Luen Yu, Chuan-Chou Shen
Publikováno v:
Geosciences, Vol 11, Iss 3, p 141 (2021)
Downcutting and infill of incised valley systems is mostly controlled by relative sea-level changes, and studies on valley-fill successions accumulated independently from relative sea-level or lake-level oscillations are limited. This study focuses o
Externí odkaz:
https://doaj.org/article/1eea679e073b442fb0659dbf85066189
Autor:
IVAN MARTINI, MAURO ALDINUCCI
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 123, Iss 3 (2017)
Basin-margin paralic deposits are sensitive indicators of relative sea-level changes and typically show complex stratigraphic architectures that only a facies-based sequence-stratigraphic approach, supported by detailed biostratigraphic data, can hel
Externí odkaz:
https://doaj.org/article/7ead66ec47304fedb28208a95df39df2
Autor:
Amalia Spina, Andrea Brogi, Enrico Capezzuoli, Gennaro Ventruti, Martina Zucchi, Mauro Aldinucci, Simonetta Cirilli, Andrea Schito, Domenico Liotta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c74cebf48300658e58dd2e442713001c
https://hdl.handle.net/11391/1538393
https://hdl.handle.net/11391/1538393
Autor:
Stefano Dominici, Luca Maria Foresi, Stefano Carnicelli, Anna Andreetta, Ivan Martini, Mauro Aldinucci, Marco Benvenuti
Publikováno v:
Sedimentary Geology. 388:99-113
The sequence-stratigraphic analysis of continental and shallow marine successions is a helpful tool for investigating the cyclicity of the sedimentary record. A similar approach is adopted in the present study to illustrate the composite cyclothemic
Autor:
Domenico Liotta, Simonetta Cirilli, Andrea Brogi, Mauro Aldinucci, Enrico Capezzuoli, Amalia Spina
Recent biostratigraphic and sedimentological studies in the inner Northern Apennines (Italy) permit to refine the upper Palaeozoic successions of southern Tuscany, allowing new hypothesis to frame these formations in the palaeogeographic scenario inh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9289402a08a7a356cbd00af719135c39
https://doi.org/10.5194/egusphere-egu21-2112
https://doi.org/10.5194/egusphere-egu21-2112
Autor:
Enrico Capezzuoli, Valeria Bianchi, Massimiliano Ghinassi, Chuan-Chou Shen, Mauro Aldinucci, Tsai-Luen Yu, Andrea Brogi
Publikováno v:
Geosciences, Vol 11, Iss 141, p 141 (2021)
Geosciences
Volume 11
Issue 3
Geosciences
Volume 11
Issue 3
Downcutting and infill of incised valley systems is mostly controlled by relative sea-level changes, and studies on valley-fill successions accumulated independently from relative sea-level or lake-level oscillations are limited. This study focuses o
Autor:
Jacopo Boaga, Rita Deiana, Mauro Aldinucci, Andrea Brogi, Valeria Bianchi, Massimiliano Ghinassi
Publikováno v:
Sedimentology. 62:897-927
Sedimentation in the upstream reaches of incised valleys is predominantly of alluvial origin and, in most cases, independent from relative sea-level or lake-level oscillations. Preserved facies distributions record the depositional response to a comb
Publikováno v:
Journal of Vertebrate Paleontology. 34:1155-1164
Geological investigation of the Boyabat Basin in north-central Anatolia, Turkey, yielded palaeoamasid (Embrithopoda, Mammalia) gnathodental fossil specimens from two localities dated to the Eocene–...
Autor:
Slavomír Nehyba, Mauro Aldinucci, Wojciech Nemec, Massimiliano Ghinassi, Volkan Özaksoy, Francesco Fidolini
Publikováno v:
Sedimentology. 61:952-977
he mode of channel-bend transformation (i.e. expansion, translation, rotation or a combination thereof) has a direct bearing on the dimensions, shape, bedding architecture and connectivity of point-bar sandstone bodies within a fluvial meander belt,
Autor:
Valeria Bianchi, Giorgia Moscon, Ivan Martini, Marcella Roner, Nicola Boscaini, Massimiliano Ghinassi, Mauro Aldinucci
Publikováno v:
Journal of Maps. 9:573-583
The study area is located across the Chianti Ridge (Tuscany, Italy), between the Upper Valdarno Basin and the Siena Basin. This area covers about 25 km2, forming a narrow belt oriented N–S and drained by the Ambra and Ombrone creeks, which flow nor