Turbidity current signature on consecutive turbidity current: analysis through numerical simulations of multiple consecutive submarine flows

Autor: Maria Azpiroz-Zabala, Joep Storms, Joris T. Eggenhuissen, Helena van der Vegt, Bert Jagers, Dirk-Jan Walstra, Arnau Obradors-Latre, Anna Pontén

Turbidity currents are powerful submarine density flows that travel towards the deep-sea carrying huge amounts of suspended sediment. The flow capacity of keeping sediment suspended in turbidity currents controls the flow duration, which can last fro

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2fdfda1d1f6a189f325cf302adf55691
https://doi.org/10.5194/egusphere-egu2020-10439

Deep-water clastic systems in the upper carboniferous (upper mississippian-lower pennsylvanian) shannon basin, western Ireland

Autor: Ole J. Martinsen, Ian A. Kane, Peter D. W. Haughton, Patrick M. Shannon, Colm Pierce, Anthea Lacchia, Trevor Elliott, Simon P. Barker, Arnau Obradors Latre, Andrew J. Pulham, George D. Sevastopulo

Publikováno v: Martinsen, O J, Pulham, A J, Elliott, T, Haughton, P, Pierce, C, Lacchia, A R, Barker, S, Latre, A O, Kane, I, Shannon, P & Sevastopulo, G D 2017, ' Deep-water clastic systems in the upper carboniferous (upper mississippian-lower pennsylvanian) shannon basin, western Ireland ', AAPG Bulletin, vol. 101, no. 4, pp. 433-439 . https://doi.org/10.1306/021417DIG17099

The Upper Carboniferous Shannon Basin of western Ireland contains amore-Than-2300-m-Thick (7540 ft) basin-fill succession, shallowing upward from deep-water to deltaic and incised fluvial deposits. The deep-water basin floor and slope succession is w

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d6ffa4ddf75b610aa84a6cfb610e5bd6
https://pure.manchester.ac.uk/ws/files/60959674/OJ_Martinsen_Shannon_Basin_AAPG_Bulletin_paper_short_version_140217.pdf