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The CMT was thicker in the study group than in the control group but this difference was not statistically significant.
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The Eocene limestone formations, which are about 100 m thick in the study area (Fig. 3), constitute a limited aquifer.
The trend to use a thicker insert in the study group suggests significantly more lateral dissection.
In our study, small regions in the right anterior inferior temporal gyrus and left ventrolateral prefrontal cortex were found to be significantly thicker, whereas in the study of Martinussen et al. (2005), cortical thickening was detected in a more superior temporal region and in the occipital lobe.
Similarly, Figure 2 shows the prevalence based on the Kato-Katz thick smear in the study locations.
However, in the present study the human cartilage thickness was 1.38 3.64 mm, thus being mostly thicker than that in the study by Öberg et al. [ 8] and in our earlier study [ 7].
Electron microscopy showed the glycocalyx to be 35 70 nm thick in this study, one to two orders of magnitude greater than the Debye length calculated for the Ringer solutions employed.
The thick sand bodies in the study area are generally present in the form of lumps.
Therefore, the thick sand bodies in the study area were deposited primarily by sandy debris flows.
No. 3 coal seam, 9 m thick is mined in the study area and the seam pitches average of 5° (Hu et al. 2016b).
The optimum yield was higher, and the aquifer was thicker, in the western part of the study area.
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