view article
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. (2014BB68).

IUCrJ
Volume 11| Part 5| September 2024| Pages 675-694
ISSN: 2052-2525
https://doi.org/10.1107/S2052252524006298