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Figure 7
The pore structure of three types of pores from Silurian black shales from the Baltic Basin, Poland, across a wide range of depths along a burial diagenetic sequence. (a) Pore characteristics of the shale rocks in their air-dried state. (b) Pore characteristics in the dehydration state after drying at 200°C. (c) Difference in pore volume between the air-dried and dehydrated states, demonstrating the structural changes induced by dehydration. This figure was adapted from Lee et al. (2014 ![]() |
IUCrJ
ISSN: 2052-2525
NEUTRON | SYNCHROTRON
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