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Nwamgba was sick with malaria that day, lying on her mud bed, rubbing her aching joints, and she asked Anikwenwa the young woman's name.
The upper prodeltaic part comprised rhythmic sequence of thin lenticular and cross-laminated sand bed and carbonaceous mud bed.
The problems and challenges involved in in situ measurement of dynamic mechanical properties of non-rigid mud bed under water wave pressure have been investigated.
The device, which is based on the analysis of the characteristics of shear wave field generated within the mud bed, was used in situ at a frequency of 619 Hz.
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The underlying unit 1b consists of abundant coarse turbidite and ash layers with mud beds.
Mud beds of Facies I can be excluded because they are thin (<0.5 m) and close to the surface (Figs. 2, 3).
As a result, most gas in the study area is regarded as being transported from gas-source beds to sand beds by formation water with the differential compaction between sand and mud beds.
Also, the capillary pressure difference between gas-source beds and sand reservoirs indicated by the huge difference in vertical permeability (Table 5) also drives gas migrating from mud beds to sandy reservoirs (cf. Magara 1987).
The dotted lines indicate the key beds (thick mud beds with diatomite, denoted as A and B, and the erosion surface of the 39-ka event shown by the large black arrow).
The lithotypes and depositional modes are: tephras (volcanic airfall); organic-rich mud (algal-rich lake sedimentation); massive to weakly graded, brown silty clay beds (homogenites and redeposited lake sediments); grey, graded sandy mud beds (intense storm-delivered sediment); and, thin yellow clay layers (run-off from small storms).
Black mud beds, defined as the Kalimati Formation (Kalimati means "black mud" in the Nepali), are widely distributed in the central part of the basin (Shrestha et al., 1998; Sakai 2001; Dill et al., 2001) and may interfinger with all the other formations (Sakai et al., 2008).
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