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The presented formulation is able to reproduce both the cross-shore profile and the distribution of sediment facies in time.
On the basis of sediment facies and modeling, the group demonstrated that the sediments were deposited in a freshwater environment, a result confirming that the subglacial meltwater network was active during the last glacial period.
Submarine landscape and sediment distribution patterns represented by five acoustic facies types represent glaciomarine sediment facies types that are related to variations in the past position and relative motion of the glacier front.
We present lake sediment facies descriptions based on data from sediment cores from two thermokarst lakes of medium depth, Claudi and Jaeger (informal names), which formed in previously non thermokarst-affected upland yedoma on the northern Seward Peninsula, Alaska.
Sediment facies and their succession combined with AMS 14C dating revealed that isochron lines cross unit boundaries clearly, and delta progradation has occurred since about 6000 to 7000 years BP, when the rising sea level neared or reached its present position.
Sediment facies analysis, electrical conductivity, and radiocarbon dating of borehole samples showed that in both cores organic-rich dark gray floodbasin mud overlies deltaic deposits dating to after approximately 3200 years calibrated radiocarbon age (cal BP) in relation to delta progradation.
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10.7554/eLife.09561.007 Figure 5. Data and characteristics of cave floor sediments (Facies 2) from the Dinaledi and Dragon's Back Chambers.
Unit 3 is composed of largely unconsolidated sediment of Facies 2 dominated by reworked orange mud clasts embedded in a brown muddy matrix.
In most side passages, where the dolomite walls narrow to thin fractures, large cascades of Flowstone 2, flow down the cave walls and spread out across the cave floor forming thin flowstone drapes on top of poorly consolidated sediment of Facies 2 containing hominin fossils (Unit 3; Figure 4F,G).
In summary, the argillic sediments of Facies III and IV are more likely to act as effective gas-source sediments (cf. Zhang and Chen 1983; Lu and Hai 1991; Wu et al. 2014).
Meanwhile, the gas sources occur as cap beds, and the mud sediments of Facies III and IV that encase sand reservoirs directly are referred as direct cap beds, while the soft mud of Facies II called indirect ones.
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