THE LOWER MARGIN OF THE SHIANT ISLES SILL

@article{Drever1958THELM,
  title={THE LOWER MARGIN OF THE SHIANT ISLES SILL},
  author={Harald Irving Drever and Robert Johnston},
  journal={Quarterly Journal of the Geological Society of London},
  year={1958},
  volume={114},
  pages={343 - 365}
}
At one locality near or at the lower margin of the main Shiant Isles sill there are contacts with Jurassic marl. Immediately adjacent to the highest of these contacts there is clear evidence of an endogenous reaction—Mg-olivine→ titanaugite. Zeolites tend to be concentrated near the contacts with marl and there is some evidence that teschenitic rock can result from exogenous reactions within the marl. An unusual degree of variability in the textural relations of olivine and augite with… Expand

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