Details
| Original language | English |
|---|---|
| Pages (from-to) | 3471-3491 |
| Number of pages | 21 |
| Journal | SEDIMENTOLOGY |
| Volume | 67 |
| Issue number | 7 |
| Early online date | 26 Apr 2020 |
| Publication status | Published - 20 Nov 2020 |
Abstract
Submarine lobes have been identified within various deep-water settings, including the basin-floor, the base of slope and the continental slope. Their dimensions and geometries are postulated to be controlled by the topographic configuration of the seabed, sediment supply system and slope gradient. Ten experiments were conducted in a three-dimensional-flume to study the depositional characteristics of submarine lobes associated with: (i) different basin floor gradients (0 to 4°); (ii) different sediment concentrations of the parent turbidity current (11 to 19% vol); and (iii) varying discharge (25 to 40 m 3 h −1). Most runs produced lobate deposits that onlapped onto the lower slope. Deposit length was proportional to basin-floor angle and sediment volume concentration. A higher amount of bypass is observed in the proximal area as the basin-floor angles get steeper and sediment concentrations higher. Deposits of runs with lower discharge could be traced higher upslope while runs with higher discharge produced an area of low deposition behind the channel mouth, i.e. discharge controlled whether lobe deposits were attached or detached from their channel-levée systems. A particle-advection-length scale analysis suggests that this approach can be used as a first order estimation of lobe element length. However, the estimations strongly depend on the average grain size used for calculations (for example, silt is still actively transported after all sand has been deposited) and the method cannot be used to locate the main depocentre. Furthermore, attempted reconstructions of turbidity current velocities from natural systems suggest that the method is not appropriate for use in inversions from more complex composite bodies such as lobes.
Keywords
- Advection length, dimensions, experimental study, morphology, sand bias, turbidity current
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Geology
- Earth and Planetary Sciences(all)
- Stratigraphy
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In: SEDIMENTOLOGY, Vol. 67, No. 7, 20.11.2020, p. 3471-3491.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - The influence of basin setting and turbidity current properties on the dimensions of submarine lobe elements
AU - Spychala, Yvonne T.
AU - Eggenhuisen, Joris T.
AU - Tilston, Mike
AU - Pohl, Florian
N1 - Funding Information: This project was funded by NWO (grant #NWO-ALW-Vidi-864.13.006), ExxonMobil, Shell and Equinor for which we are thankful. Thony van der Gon-Netscher and Han de Witte supplied technical support to the experimental work. Reviews by Sedimentology Associate Editor Kyle Straub and reviewer Elisabeth Steel greatly improved the manuscript. Open access funding enabled and organized by Projekt DEAL.
PY - 2020/11/20
Y1 - 2020/11/20
N2 - Submarine lobes have been identified within various deep-water settings, including the basin-floor, the base of slope and the continental slope. Their dimensions and geometries are postulated to be controlled by the topographic configuration of the seabed, sediment supply system and slope gradient. Ten experiments were conducted in a three-dimensional-flume to study the depositional characteristics of submarine lobes associated with: (i) different basin floor gradients (0 to 4°); (ii) different sediment concentrations of the parent turbidity current (11 to 19% vol); and (iii) varying discharge (25 to 40 m 3 h −1). Most runs produced lobate deposits that onlapped onto the lower slope. Deposit length was proportional to basin-floor angle and sediment volume concentration. A higher amount of bypass is observed in the proximal area as the basin-floor angles get steeper and sediment concentrations higher. Deposits of runs with lower discharge could be traced higher upslope while runs with higher discharge produced an area of low deposition behind the channel mouth, i.e. discharge controlled whether lobe deposits were attached or detached from their channel-levée systems. A particle-advection-length scale analysis suggests that this approach can be used as a first order estimation of lobe element length. However, the estimations strongly depend on the average grain size used for calculations (for example, silt is still actively transported after all sand has been deposited) and the method cannot be used to locate the main depocentre. Furthermore, attempted reconstructions of turbidity current velocities from natural systems suggest that the method is not appropriate for use in inversions from more complex composite bodies such as lobes.
AB - Submarine lobes have been identified within various deep-water settings, including the basin-floor, the base of slope and the continental slope. Their dimensions and geometries are postulated to be controlled by the topographic configuration of the seabed, sediment supply system and slope gradient. Ten experiments were conducted in a three-dimensional-flume to study the depositional characteristics of submarine lobes associated with: (i) different basin floor gradients (0 to 4°); (ii) different sediment concentrations of the parent turbidity current (11 to 19% vol); and (iii) varying discharge (25 to 40 m 3 h −1). Most runs produced lobate deposits that onlapped onto the lower slope. Deposit length was proportional to basin-floor angle and sediment volume concentration. A higher amount of bypass is observed in the proximal area as the basin-floor angles get steeper and sediment concentrations higher. Deposits of runs with lower discharge could be traced higher upslope while runs with higher discharge produced an area of low deposition behind the channel mouth, i.e. discharge controlled whether lobe deposits were attached or detached from their channel-levée systems. A particle-advection-length scale analysis suggests that this approach can be used as a first order estimation of lobe element length. However, the estimations strongly depend on the average grain size used for calculations (for example, silt is still actively transported after all sand has been deposited) and the method cannot be used to locate the main depocentre. Furthermore, attempted reconstructions of turbidity current velocities from natural systems suggest that the method is not appropriate for use in inversions from more complex composite bodies such as lobes.
KW - Advection length
KW - dimensions
KW - experimental study
KW - morphology
KW - sand bias
KW - turbidity current
UR - http://www.scopus.com/inward/record.url?scp=85085618414&partnerID=8YFLogxK
U2 - 10.1111/sed.12751
DO - 10.1111/sed.12751
M3 - Article
VL - 67
SP - 3471
EP - 3491
JO - SEDIMENTOLOGY
JF - SEDIMENTOLOGY
SN - 0037-0746
IS - 7
ER -