Submarine crevasse lobes controlled by lateral slope failure in tectonically-active settings: an exhumed example from the Eocene Aínsa depocentre (Spain)

Autor: Ander Martinez-Doñate, Euan L. Soutter, Ian A. Kane, Miquel Poyatos-Moré, David M. Hodgson, Ashley J. M. Ayckbourne, William J. Taylor, Max J. Bouwmeester, Stephen S. Flint

Publikováno v: Sedimentologika, Vol 1, Iss 1 (2023)

Tectonic deformation and associated submarine slope failures modify seafloor relief, influencing sediment dispersal patterns and the resulting depositional architecture of deep-water systems. The exhumed Middle Eocene strata of the Banastón deep-wat

Externí odkaz: https://doaj.org/article/0eff0d614f14427f817569055d7d221b

Stratigraphic change in flow transformation processes recorded in early post‐rift deep‐marine intraslope lobe complexes

Autor: Ander Martinez‐Doñate, Ian A. Kane, David M. Hodgson, Aurelia M.‐L. J. Privat, Christopher A.‐L. Jackson, Ernesto Schwarz, Stephen S. Flint

Publikováno v: Martinez-Doñate, A, Kane, I A, Hodgson, D M, Privat, A M L J, Jackson, C A L, Schwarz, E & Flint, S S 2023, ' Stratigraphic change in flow transformation processes recorded in early post-rift deep-marine intraslope lobe complexes ', Sedimentology . https://doi.org/10.1111/sed.13086

The Early Jurassic Los Molles Formation in the Neuquén Basin of western Argentina is a rare example of well-exposed syn-rift to post-rift stratigraphy. In the Chachil Graben, the onset of the early post-rift stage is marked by drowning of a carbonat

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48b62833aad0bec462ba747623689294
https://doi.org/10.1111/sed.13086

Fringe or background: Characterizing deep-water mudstones beyond the basin-floor fan sandstone pinchout

Autor: Miquel Poyatos-Moré, David M. Hodgson, Kévin Boulesteix, Kevin G. Taylor, Stephen S. Flint

Publikováno v: Journal of Sedimentary Research. 90:1678-1705

Mud dominates volumetrically the fraction of sediment delivered and deposited in deep-water environments, and mudstone is a major component of basin-floor successions. However, studies of basin-floor deposits have mainly focused on their proximal san

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a0e6296b09cb61730cd1e70758a1b553
https://doi.org/10.2110/jsr.2020.048

Substrate Entrainment, Depositional Relief, and Sediment Capture: Impact of a Submarine Landslide on Flow Process and Sediment Supply

Autor: Christopher A.-L. Jackson, Ander Martinez-donate, Christopher J. Stevenson, Edward Keavney, David M. Hodgson, Robert Anthony Duller, Aurélia Privat, Stephen S. Flint, Ian A. Kane, Ernesto Schwarz, Yvonne T. Spychala

Publikováno v: CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Frontiers in Earth Science, Vol 9 (2021)
Martínez-Doñate, A, Privat, A M L J, Hodgson, D M, Jackson, C A L, Kane, I A, Spychala, Y T, Duller, R A, Stevenson, C, Keavney, E, Schwarz, E & Flint, S S 2021, ' Substrate Entrainment, Depositional Relief, and Sediment Capture : Impact of a Submarine Landslide on Flow Process and Sediment Supply ', Frontiers in Earth Science, vol. 9, 757617 . https://doi.org/10.3389/feart.2021.757617
FRONTIERS IN EARTH SCIENCE
Martínez-Doñate Gomez, A, Privat, A M L J, Hodgson, D, Kane, I, Jackson, C, Stevenson, C, Duller, R A, Spychala, Y T, Keavney, E & Flint, S 2021, ' SUBSTRATE ENTRAINMENT, DEPOSITIONAL RELIEF, AND SEDIMENT CAPTURE: IMPACT OF A SUBMARINE LANDSLIDE ON FLOW PROCESS AND SEDIMENT SUPPLY ', Frontiers in Earth Science, vol. 9 . https://doi.org/10.3389/feart.2021.757617

Submarine landslides can generate complicated patterns of seafloor relief that influence subsequent flow behaviour and sediment dispersal patterns. In subsurface studies, the term mass transport deposits (MTDs) is commonly used and covers a range of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9edac3e9882edee2a7d15451315d8ddc
https://doi.org/10.3389/feart.2021.757617

Interpretation of mouth-bar and related lacustrine and fluvial sand bodies from the middle Green River Formation (Eocene), southern Uinta Basin, Utah

Autor: John A. Howell, Dave Keighley, Øystein Spinnangr, Stephen S. Flint

The Uinta Basin of eastern Utah is an intermontane basin that contains an ~2-km-thick succession of mostly carbonate-rich mudrock assigned to the Eocene Green River Formation. In the southwest part of the basin, along Nine Mile Canyon and its tributa

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::18dccad77832d5caf6f1703cc7eeebda
https://doi.org/10.1130/2019.2536(15)