Tempestite facies variability and storm‐depositional processes across a wide ramp: Towards a polygenetic model for hummocky cross‐stratification
The hydrodynamic mechanisms responsible for the genesis and facies variability of shallow‐
marine sandstone storm deposits (tempestites) have been intensely debated, with particular …
marine sandstone storm deposits (tempestites) have been intensely debated, with particular …
Tempestite deposition
PM Myrow, JB Southard - Journal of Sedimentary …, 1996 - pubs.geoscienceworld.org
A model is developed to explain the wide range of sedimentary structures found in ancient
storm-deposited beds. The model predicts the nature and association of internal …
storm-deposited beds. The model predicts the nature and association of internal …
Distinctive features of sandy tempestites
A Seilacher - Cyclic and event stratification, 1982 - Springer
Distinctive Features of Sandy Tempestites Page 1 Distinctive Features of Sandy Tempestites A.
SEILACHER Abstract: Sedimentological and biological features allow to distinguish …
SEILACHER Abstract: Sedimentological and biological features allow to distinguish …
Experiments on oscillatory-flow and combined-flow bed forms: implications for interpreting parts of the shallow-marine sedimentary record
S Dumas, RWC Arnott… - Journal of …, 2005 - pubs.geoscienceworld.org
Analog laboratory experiments were conducted to investigate subaqueous bed forms
generated under storm-like oscillatory and combined flow. Experiments were carried out in a …
generated under storm-like oscillatory and combined flow. Experiments were carried out in a …
Model for the combined-flow origin of hummocky cross-stratification
A Nøttvedt, RD Kreisa - Geology, 1987 - pubs.geoscienceworld.org
Many shallow marine sandstones are characterized by gently dipping trough cross-
stratification. There appear to be significant similarities between this low-angle cross …
stratification. There appear to be significant similarities between this low-angle cross …
Origin of hummocky and swaley cross-stratification—The controlling influence of unidirectional current strength and aggradation rate
S Dumas, RWC Arnott - Geology, 2006 - pubs.geoscienceworld.org
A series of wave-tunnel experiments was conducted to investigate the conditions under
which hummocky and swaley cross-stratification form. Isotropic 3-dimensional (3-D) …
which hummocky and swaley cross-stratification form. Isotropic 3-dimensional (3-D) …
The role of shelf morphology on storm‐bed variability and stratigraphic architecture, Lower Cretaceous, Svalbard
The dominance of isotropic hummocky cross‐stratification, recording deposition solely by
oscillatory flows, in many ancient storm‐dominated shoreface–shelf successions is …
oscillatory flows, in many ancient storm‐dominated shoreface–shelf successions is …
Temporal variation in the wavelength of hummocky cross-stratification: Implications for storm intensity through Mesozoic and Cenozoic
M Ito, A Ishigaki, T Nishikawa, T Saito - Geology, 2001 - pubs.geoscienceworld.org
Hummocky cross-stratification is believed to be one of the diagnostic sedimentary structures
of storm-dominated shallow-marine environments. The wavelength of this stratification …
of storm-dominated shallow-marine environments. The wavelength of this stratification …
Bypass-zone tempestite facies model and proximality trends for an ancient muddy shoreline and shelf
PM Myrow - Journal of Sedimentary research, 1992 - pubs.geoscienceworld.org
Member 2 of the late Precambrian to Lower Cambrian Chapel Island Formation of southeast
Newfoundland was primarily deposited in storm-influenced, nearshore and shelf …
Newfoundland was primarily deposited in storm-influenced, nearshore and shelf …
Is most hummocky cross‐stratification formed by large‐scale ripples?
JG Quin - Sedimentology, 2011 - Wiley Online Library
Although normal isotropic hummocky cross‐stratification is commonly interpreted to be the
deposit of large‐scale ripples, there are many reasons why this may not usually be the case …
deposit of large‐scale ripples, there are many reasons why this may not usually be the case …
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