The increase in average thickness parameter reflects the increase in crack length. But, the crack density parameter decreases drastically. It implies that number of cracks are drastically decreased. The crack length is more than twice of that at pressure of 1.0GPa (Fig. 5 c). Possibly, most of small cracks are closed under pressure. Furthermore, the cracks are more long, sparse and deep, compared with cracks at atmospheric pressure. This can be inferred from the increase of fracture volume and texture.
The presence of much oil shale suggests that there are many crack-like structures in a rock. The crack-like structures have long and deep cracks, however, their lengths are much shorter than the size of the rock samples.
The increase of volume can be attributed to the closure of cracks. The fracture volume is more than twice that of the one at atmospheric pressure. The increase in fraction of brittle fracture indicates the closure of cracks. Brittle fractures are dominant in the sample at pressure of 1.0GPa.
The increase in oil shale yield of a fine-grained sedimentary rock indicates that the permeability of fine-grained sedimentary rocks is enhanced by the consolidation of fractures. The pore structure is well measured by X-ray CT images. There are many wide pores interconnected by cracks. In a rock, many cracks make the connectivity of brine within a rock. Interconnected pores can easily keep brine in a rock and promote fluid migration. Therefore, the oil shale yield of the rock is enhanced.
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