A New Type of Bedform Produced by Backfilling Processes in a Submarine Channel, Late Miocene, Tabernas-Sorbas Basin, SE Spain

Abstract

The Late Miocene ''Solitary Channel,'' Tabernas-Sorbas basin, SE Spain, has been interpreted as a submarine channel fed by sediment gravity flows from the east. In this paper, the channel is reinterpreted as a lower-slope erosional channel fed by sediment gravity flows from the west. The channel shows cobble/pebble lag deposits, including breccias, associated with erosional phases with substantial sediment bypass, and a later infill by episodes of inclined backstepping macroforms (the primary focus in this paper), mainly comprising sands, interpreted here for the first time as channel backfill deposits. These inclined sandy macroforms, typically 2-5 m in height and 30-40 m in length, are described in detail for the first time in this paper, and are interpreted as a new large-scale sedimentary structure. We observe that the seeding process for the inclined sandy macroforms appears to have been in the upstream depression immediately behind ridges on the surface directly overlying cohesive debris-flow deposits.The internal channel architecture is interpreted in terms of fluctuating relative base levels. A purely local tectonic explanation for the inclined sandy macroforms is discounted because within the bed bundles, dips are essentially constant across the intrachannel disconformities. We speculate that the most likely overall change in base level throughout the history of the channel was driven by regional tectonic change. The higher-frequency variations were probably a consequence of fluctuations in sediment supply/caliber from the source area and/or of cycles of eustatic or regional sea-level changes. The channel was abruptly overlain by about 200 m of marls and then a heterolithic sheet-like turbidite system typical of a confined basin-floor setting. This change in depositional style represents a response to a significant overall decrease in basin-floor gradient, in which there was a differential change in base level, shown by the coeval development of a major angular unconformity farther east (Sorbas area). The channel history is important for sequence-stratigraphic modeling because it demonstrates that a backstepping fill can be caused by an overall tectonic control on the accommodation space (initiation and abandonment). Higher-frequency source-area changes in sediment flux/caliber and/or eustatic sea level probably exert a strong influence on the detailed depositional architecture in the channel (multiple bypass-backfill events).

Late Quaternary palaeosols in the Yangtze Delta, China, and their palaeoenvironmental implications

“…The preferred orientation of magnetic minerals revealed by AMS measurement has been used to infer hydrodynamic processes during their deposition (Rees, 1965;Taira and Lienert 1979;Pickering et al, 1992). AMS investigation has proved useful in identifications of palaeoflow direction (e.g., Rusnak, 1957;Ellwood and Ledbetter, 1977;Pickering et al, 1992Pickering et al, , 2001, and in differentiating late Quaternary coastal sedimentary environments (e.g., Chen et al, 1998;Liu et al, 2001Liu et al, , 2005. The AMS technique has been applied comprehensively in studies of sediments from various environments, such as loess (Liu et al, 1990;Lagroix and Banerjee, 2002;Zhu et al, 2004), tidal flat sediments (Cong et al, 1997;Chen et al, 1998), lake sediments (Rosenbaum et al, 2000;Schneider et al, 2004), and fluvial deposits (Sangode et al, 2001;Zhang et al, 2004).…”

Quantitative Seismic Geomorphology of a Confined Channel Complex, Southern Atwater Fold Belt, Gulf of Mexico, U.S.A.

“…This view is consistent with the description of flow stripping and outer channel margin sand lens deposition presented in Clark and Pickering (1996). Medial Accretion, also known as Straight Course/Gentle Upcurrent Accretion or Backstepping Inclined Sandy Macroform accretion, occurs as fans backstep and translate updip due to changes in channel gradient (Pickering et al, 2001). These sub-valley scale features are an important target of research for this study.…”

Combined tectonic-sediment supply-driven cycles in a Lower Carboniferous deep-marine foreland basin, Moravice Formation, Czech Republic

“…2, 3), sometimes consisting of higher-order, metrescale FU cycles. Although FU cycles are characteristic features of turbidite systems in general and may occur both in confined and unconfined turbidite successions (Mutti 1992), such cycles have been mostly interpreted as filling confined channel forms and reflecting channel progressive abandonment, migration or upslope filling (Bouma et al 1985;Mutti 1992;Pickering et al 2001;Hickson and Lowe 2002). Similarly, blocky cycles indicate channel migration or channel abandonment (Surlyk 1987).…”