<abstract xmlns="http://www.w3.org/1999/xhtml"><p>The silty top parts of graded turbidites of the Late Ordovician Pingliang Formation, which accumulated along the southern margin of the Ordos Basin (central China), have been reworked by contour currents. The reworking of the turbidites can be proven on the basis of paleocurrent directions in individual layers: the ripple-cross-bedded sandy divisions of some turbidites show transport directions consistently into the downslope direction (consistent with the direction of other gravity flows), but in the upper, silty fine-grained division they show another direction, viz. alongslope (consistent with the direction that a contour current must have taken at the same time). Both directions are roughly perpendicular to each other. Moreover, the sediment of the reworked turbidites is better sorted and has better rounded grains than the non-reworked turbidites.</p><p>Although such type of reworking is well known from modern deep-sea environments, this has rarely been found before in ancient deep-sea deposits. The reworking could take place because the upper divisions of the turbidites involved are silty and consequently relatively easily erodible, while the contour current had locally a relatively high velocity – and consequently a relatively large erosional capability – because of confinement within a relatively narrow trough.</p></abstract>

The silty top parts of graded turbidites of the Late Ordovician Pingliang Formation, which accumulated along the southern margin of the Ordos Basin (central China), have been reworked by contour currents. The reworking of the turbidites can be proven on the basis of paleocurrent directions in individual layers: the ripple-cross-bedded sandy divisions of some turbidites show transport directions consistently into the downslope direction (consistent with the direction of other gravity flows), but in the upper, silty fine-grained division they show another direction, viz. alongslope (consistent with the direction that a contour current must have taken at the same time). Both directions are roughly perpendicular to each other. Moreover, the sediment of the reworked turbidites is better sorted and has better rounded grains than the non-reworked turbidites.Although such type of reworking is well known from modern deep-sea environments, this has rarely been found before in ancient deep-sea deposits. The reworking could take place because the upper divisions of the turbidites involved are silty and consequently relatively easily erodible, while the contour current had locally a relatively high velocity – and consequently a relatively large erosional capability – because of confinement within a relatively narrow trough.

Interaction between turbidity currents and a contour current – A rare example from the Ordovician of Shaanxi province, China

Shandong University of Science and Technology

Geologos

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

The silty top parts of graded turbidites of the Late Ordovician Pingliang Formation, which accumulated along the southern margin of the Ordos Basin (central...

Interaction between turbidity currents and a contour current – A rare example from the Ordovician of Shaanxi province, China

Publicado en línea: 13 jun 2019

Páginas: 15 - 30

Recibido: 25 ago 2018

Aceptado: 15 ene 2019

DOI: https://doi.org/10.2478/logos-2019-0002

Palabras clave
contourites, turbidites, reworking, Ordos Basin, Pingliang Formation

© 2019 Hua Li et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Interaction between turbidity currents and a contour current – A rare example from the Ordovician of Shaanxi province, China

Publicado en línea: 13 jun 2019

Páginas: 15 - 30

Recibido: 25 ago 2018

Aceptado: 15 ene 2019

DOI: https://doi.org/10.2478/logos-2019-0002

Palabras clavecontourites, turbidites, reworking, Ordos Basin, Pingliang Formation

© 2019 Hua Li et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Palabras clave
contourites, turbidites, reworking, Ordos Basin, Pingliang Formation