A Source-to-Sink Compositional Model of a Present Highstand: An Example in the Low-Rank Tiber Depositional Sequence (Latium Tyrrhenian Margin, Italy)
作者： Daniel Tentori , Salvatore Milli , Kathleen M. Marsaglia
DOI: 10.2110/JSR.2018.60
关键词:
摘要: Abstract Our source-to-sink compositional model of sediment distribution in the present highstand Tiber Depositional Sequence has important implications for source lithology, generation, transport, and deposition. In River system, sand trends reflect provenance mixing, anthropic intervention, effects local autogenic factors continental to marine depositional environments. Fluvial feldspatho-quartzo-lithic results from contribution major tributaries drainage basin, which can be divided into two sub-basins separated by Corbara dam built 1950s. Upstream-drainage-basin a siliciclastic sedimentary lithic signature, whereas carbonate volcanic fragments dominate downstream-drainage-basin sand. Downstream is further modified coastal environment hydraulic sorting, mixed with detritus derived recycling dune altered volcaniclastic paleosols. The latter are associated lower-course floodplain channel deposits, produce quartzo-feldspatho-lithic Sediment grain-size zonation influenced hydrodynamics, which, turn, detrital populations distinct signatures behavior. Coarser minerals (essentially pyroxene phenocrysts) finer feldspar grains progressively concentrated higher-energy lower-energy environments, respectively. Biogenic shelf slope deposits off mouth show very little riverine influence. This study last system tract clarifies dependence, reworking controlling final composition modern knowledge used better understand modes ancient successions.
geoscienceworld.org
harvard.edu
sci-hub.se 参考文章(78)
Gian Gaspare Zuffa, Optical Analyses of Arenites: Influence of Methodology on Compositional Results Springer, Dordrecht. pp. 165- 189 ,(1985) , 10.1007/978-94-017-2809-6_8
Alessandro Amorosi, Gian Gaspare Zuffa, Sand composition changes across key boundaries of siliciclastic and hybrid depositional sequences Sedimentary Geology. ,vol. 236, pp. 153- 163 ,(2011) , 10.1016/J.SEDGEO.2011.01.003
S.J. Bentley, M.D. Blum, J. Maloney, L. Pond, R. Paulsell, The Mississippi River source-to-sink system: Perspectives on tectonic, climatic, and anthropogenic influences, Miocene to Anthropocene Earth-Science Reviews. ,vol. 153, pp. 139- 174 ,(2016) , 10.1016/J.EARSCIREV.2015.11.001
Kathleen M. Marsaglia, 9. PETROGRAPHY AND PROVENANCE OF VOLCANICLASTIC SANDS RECOVERED FROM THE IZU-BONIN ARC, LEG 1261 ,(1992)
Palynology and Mediterranean vegetation history FLORA MEDITERRANEA. ,vol. 23, pp. 141- 156 ,(2013) , 10.7320/FLMEDIT23.141
Pieter Vermeesch, Alberto Resentini, Eduardo Garzanti, An R package for statistical provenance analysis Sedimentary Geology. ,vol. 336, pp. 14- 25 ,(2016) , 10.1016/J.SEDGEO.2016.01.009
R. Funiciello, A Trigari, A Esposito, C Rosa, Guido Giordano, I Mazzini, M Fabbri, D De Rita, The sedimentation along the Roman coast between Middle and Upper Pleistocene: the interplay of eustatism, tectonics and volcanism – new data and review ,vol. 16, pp. 121- 129 ,(2002)
Hanane Reddad, Hajar El Talibi, Francesco Perri, Said El Moussaoui, Mohamed Amine Zerdeb, Mohamed Najib Zaghloul, Salvatore Critelli, Textural and compositional controls on modern fluvial and beach sands of Mediterranean coastal Rif belt (Northern Rif, Morocco) Bollettino Della Societa Geologica Italiana. ,vol. 135, pp. 336- 349 ,(2016) , 10.3301/IJG.2015.33
Leopoldo Franco, Sander Boer, Andrea Ferrante, MODELLING AND MONITORING OF A PERCHED BEACH AT LIDO DI OSTIA (ROME) 23rd International Conference on Coastal Engineering. ,vol. 1, pp. 3305- 3318 ,(1993) , 10.9753/ICCE.V23.%P
M Dane Picard, Earle F McBride, None, Comparison of river and beach sand composition with source rocks, Dolomite Alps drainage basins, northeastern Italy Geological Society of America Special Papers. ,vol. 420, pp. 1- 12 ,(2007) , 10.1130/2007.2420(01)