The Oil-Shales of the Lothians. Pt. I. the Geology of the Oil-Shale Fields, By R. G. Carruthers, Based On the Work of H. M. Cadell And J. S. Grant Wilson. Pt. Ii. Methods of Working the Oil-Shales, By W. Caldwell. Pt. Iii. the Chemistry of the Oil-Shales,
The book The Oil-Shales of the Lothians. Pt. I. the Geology of the Oil-Shale Fields, By R. G. Carruthers, Based On the Work of H. M. Cadell And J. S. Grant Wilson. Pt. Ii. Methods of Working the Oil-Shales, By W. Caldwell. Pt. Iii. the Chemistry of the Oil-Shales, was written by author Geological Survey of Great Britain Here you can read free online of The Oil-Shales of the Lothians. Pt. I. the Geology of the Oil-Shale Fields, By R. G. Carruthers, Based On the Work of H. M. Cadell And J. S. Grant Wilson. Pt. Ii. Methods of Working the Oil-Shales, By W. Caldwell. Pt. Iii. the Chemistry of the Oil-Shales, book, rate and share your impressions in comments. If you don't know what to write, just answer the question: Why is The Oil-Shales of the Lothians. Pt. I. the Geology of the Oil-Shale Fields, By R. G. Carruthers, Based On the Work of H. M. Cadell And J. S. Grant Wilson. Pt. Ii. Methods of Working the Oil-Shales, By W. Caldwell. Pt. Iii. the Chemistry of the Oil-Shales, a good or bad book?
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There seems to be a general law, not without exceptions, that shales deteriorate with depth. This featm'e is very marked in the Linlithgow district in the case of the Broxbm'n seam ; very distinct but not so acute at Broxburn, much less apparent at Oakbank, while at Pentland increase of depth does not seem to diminish the yield of oil at all. This deterioration with depth is gTeatest towards the north, and it decreases towards the south. The kerogen may be amenable to pressure under heat and sl...ightly mobile, but we must remember that the present thicloiess of strata at any particular point is no indication of the thickness in past geological time ; and fm'ther, we should bear in mind that a great load of overlying materials probably implied increased temperatm*e. If pressure be looked on as the cause of the decrease in oil with depth, then some accidental circumstance has in certain cases increased the pressure near the outcrop, and in others diminished it at greater depths. During the folding and faulting that took place long after the deposition of the sediments this might sometimes have happened.
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