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These different surfaces can be time-equivalent along the basin margin.
The sequence was deposited as alluvial fan fan-delta complexes, controlled by basin margin fan fan-delta
The abrupt lithofacies boundary between the early and later diatreme fills and the proximity of the diatreme to the basin margin suggests that the migration was caused by an abrupt tectonic activity near the basin margin.
In the long term, the depositional evolution from DS1 to DS3 reveals basin margin progradation associated with decreasing siliciclastic supply.
Element I occurs along the basin margin and shows a monotonous stacking of tabular or crudely stratified conglomeratic units.
Surface uplift along the eastern basin margin coincides with a rapid increase in plant transpiration in response to reduced moisture supply into the AB (Fig. 3).
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Variations in the distribution of the clay mineral cement correlate to the increased occurrence of fractures and disaggregation bands towards the salt wall at the mini-basin margin (Fig. 4).
The higher density of disaggregation bands at the mini-basin margin can also complicate fluid flow and reservoir quality prediction as fractures, faults and disaggregation bands create a complex system of permeable fluid pathways and cemented baffles at deeper burial (e.g. Fossen et al. 2007).
The northwestern part of Kyongsang Basin (Early Cretaceous) largely comprises interbedded sandstones and mudstones of fluvial depositional environments with local basin-margin conglomeratic deposits of alluvial fan systems.
Reconstruction of the depositional geometry of the Tyee Basin succession from detailed outcrop and subsurface data reveals two distinct stages of development for this active basin-margin.
Slope-channel topography facilitated the development of relatively coarse-grained, amalgamated turbidite reservoirs, whereas unchannelized basin-margin topography facilitated deposition of fine-grained, chaotic non-reservoirs.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com