Sentence examples for sedimentary supply from inspiring English sources

Non-synchronous stacking patterns can form when the accommodation space increment (∆A) is less than that of sedimentary supply (∆S) in one area, but larger than or equal to that of ∆S in another.

This fluvial sensitivity to the meteorological conditions induced temporal variations in sedimentary supply originating from either direct input from remnants of periglacial alluvial sheets or local rocky outcrops and/or from indirect input from the erosion of alluvial and colluvial deposits.

Otherwise, in times of rising sea level where sedimentary supply is scarce, turbidite channel systems are seldom developed.

Because of the contemporaneous falling sea level and continent uplifting, it reduces the distance between provenance and deepwater sedimentary supply, which is beneficial to form sediments.

Due to the effects of allocyclic factors, such as lake level rising, accommodation space, and sedimentary supply rate, the main evolutionary mode of the composite sand body is vertical overlaying, which includes diverse modes such as progradation, retrogradation, and aggradation.

In contrast, during lake filling, the accommodation space increases due to the decreasing of sedimentary supply, and the shapes of the sand bodies transition from single and multiple blocks to streaks and dendrites with decreasing width and thickness.

In doing so, we provide a benchmark against which to compare older deposits within the East China Sea and other Chinese sedimentary basins supplied by the Yangtze.

Obvious sources for particulate materials for the 15°N band are the Fonta-Djalon highlands which supply sedimentary material to the River Niger; the Bodele Depression, the deepest part of Lake Megachad, source of dust for the World; the Ethiopian highlands at the eastern end of 15°N which supply silt to the Nile system and particulates to the 15°N region.

Major drainage systems entered the Fushan Depression through the accommodation zone along the direction of sediment supply, and sedimentary flow paths were parallel to the accommodation zone axis with sedimentary flows constrained to the adjacent areas of the NW-trending transfer faults.

Variations in the amount of precipitation were the predominant allocyclic control on stratigraphic variations in terrestrial organic productivity, lacustrine base levels, basin-scale weathering, water table and pedogenesis, sediment supply, and sedimentary geochemistry.

In the Mejillones Formation, a shallow-marine Pleistocene succession of northern Chile, the cyclic stratigraphic record is the result of the complex interaction of regional uplift, glacio-eustasy, local tectonics, sediment supply, and sedimentary processes.