Sole marks reveal deep-marine depositional process and environment: Implications for flow transformation and hybrid-event-bed models
Deposits of sediment gravity flows in the Aberystwyth Grits Group (Silurian, west Wales,
United Kingdom) display evidence that sole marks are suitable for reconstructing …
United Kingdom) display evidence that sole marks are suitable for reconstructing …
Hybrid event bed character and distribution in the context of ancient deep‐lacustrine fan models
Hybrid event beds are texturally and compositionally‐diverse deposits preserved within
deepwater settings. They are deposited by flows exhibiting 'mixed behaviour', forming …
deepwater settings. They are deposited by flows exhibiting 'mixed behaviour', forming …
An integrated process‐based model of flutes and tool marks in deep‐water environments: Implications for palaeohydraulics, the Bouma sequence and hybrid event …
Flutes and tool marks are commonly observed sedimentary structures on the bases of
sandstones in deep‐water successions. These sole structures are universally used as …
sandstones in deep‐water successions. These sole structures are universally used as …
Channel‐lobe transition zone development in tectonically active settings: Implications for hybrid bed development
Channel‐lobe transition zones are dynamic areas located between deepwater channels
and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone …
and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone …
Integrating transitional-flow signatures into hybrid event beds: implications for hybrid-flow evolution on a submarine lobe fringe
Alongside turbidites and debrites, hybrid event beds are now recognized as a common
occurrence in deep-marine environments. Yet, many variations in the standard H1–H5 …
occurrence in deep-marine environments. Yet, many variations in the standard H1–H5 …
Mixed axial and transverse deep‐water systems: The Cretaceous post‐rift Lysing Formation, offshore Norway
LAS Hansen, DM Hodgson, A Pontén, C Thrana… - Basin …, 2021 - earthdoc.org
Deep‐water stratigraphic successions from syn‐to post‐rift stages are an archive of evolving
physiographic configurations, and can record axial and transverse sedimentary sources …
physiographic configurations, and can record axial and transverse sedimentary sources …
[HTML][HTML] Quantification of basin-floor fan pinchouts: examples from the Karoo Basin, South Africa
LAS Hansen, DM Hodgson, A Pontén, D Bell… - Frontiers in Earth …, 2019 - frontiersin.org
The topography of the seabed (orientation and gradient) and rheology of the flows greatly
influences the character of basin-floor turbidity current deposits. Therefore, submarine fan …
influences the character of basin-floor turbidity current deposits. Therefore, submarine fan …
Facies heterogeneity and lobe facies multiscale analysis of deep-marine sand-shale complexity in the West Crocker Formation of Sabah Basin, NW Borneo
Featured Application A generalized conceptual model for the characterization of a deep-
marine siliciclastic complex deposition with respect to the integrated submarine fan and lobe …
marine siliciclastic complex deposition with respect to the integrated submarine fan and lobe …
Topographic controls on the development of contemporaneous but contrasting basin-floor depositional architectures
Sediment-laden gravity-driven-flow deposits on the basin floor are typically considered to
form either discrete lobes that stack compensationally, or packages of laterally extensive …
form either discrete lobes that stack compensationally, or packages of laterally extensive …
Syn‐rift mass flow generated 'tectonofacies' and 'tectonosequences' of the Kingston Peak Formation, Death Valley, California, and their bearing on supposed …
Abstract The Kingston Peak Formation of the Pahrump Group in the Death Valley region of
the Basin and Range Province, USA, is the thick (over 3 km) mixed siliciclastic–carbonate fill …
the Basin and Range Province, USA, is the thick (over 3 km) mixed siliciclastic–carbonate fill …