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Proximal to distal grain-size distribution of basin-floor lobes: A study from the Battfjellet Formation, Central Tertiary Basin, Svalbard

2021 Score: 35 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Florian Pohl Florian Pohl Florian Pohl Florian Pohl Florian Pohl Florian Pohl Yvonne Spychala, Florian Pohl Florian Pohl Yvonne Spychala, Joris T. Eggenhuisen, Thymen Ramaaker, Thymen Ramaaker, Florian Pohl Joris T. Eggenhuisen, Joris T. Eggenhuisen, Joris T. Eggenhuisen, Joris T. Eggenhuisen, Florian Pohl Florian Pohl Joris T. Eggenhuisen, Joris T. Eggenhuisen, Sten‐Andreas Grundvåg, Sten‐Andreas Grundvåg, Florian Pohl Florian Pohl Yvonne Spychala, Florian Pohl Joris T. Eggenhuisen, Florian Pohl Sara Wroblewska, Sara Wroblewska, Joris T. Eggenhuisen, Joris T. Eggenhuisen, Florian Pohl Florian Pohl Florian Pohl Yvonne Spychala, Florian Pohl Joris T. Eggenhuisen, Florian Pohl Florian Pohl

Summary

Geologists studied the grain-size distribution in deep-sea sediment deposits to understand how underwater flows transport and deposit particles. This sedimentology study contributes to understanding how microplastics — which behave as particles in ocean currents — distribute and settle on the seafloor.

Study Type Environmental

The grain-size distribution of sediment particles is an important aspect of the architecture of submarine fans and lobes. It governs depositional sand quality and reflects distribution of particulate organic carbon and pollutants. Documenting the grain-size distribution of these deep-marine sedimentary bodies can also offer us an insight into the flows that deposited them. Submarine lobes are commonly assumed to linearly fine from an apex, meaning there should be a proportional relationship between grain size and distance from the lobe apex. However, not much detailed quantitative work has been done to test this hypothesis. Exposure of a 5 km long dip-section of basin-floor lobes in Clinoform 12, Battfjellet Formation, Spitsbergen, enable the study of basinward grain-size evolution in lobe deposits. Furthermore, the dataset allows testing if there are any documentable grain-size differences between lobe sub-environments. For this purpose, the palaeogeography of Clinoform 12 was reconstructed and the youngest lobe, which was exposed in all collected logs, chosen to be evaluated for its grain-size trends. Photographed thin-sections of 66 rock samples were analysed to obtain quantitative grain-size distributions. The results show that fining of lobe deposits occurs predominantly in the most proximal and most distal parts of the lobe, while the intermediate lobe, which is dominated by lobe off-axis deposits, is characterised by a relatively consistent grain-size range. Lobe sub-environments show statistically distinct grain-size distributions from lobe axis to lobe fringe. An explanation for these trends is the interplay of capacity and competence-driven deposition with the grain-size stratification of the flows. The outcomes of this study help to better understand the proximal to distal evolution of turbidity currents and their depositional patterns. They also provide important insights in reservoir potential of basin-floor fans at lobe scale.

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