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Results of refraction work in the northern Irish Sea confirm the presence of sedimentary basins of presumed Permo-Triassic age in the Solway Firth and the eastern Irish Sea. A gravity low west of the Isle of Man is, however, more probably largely due to a granite.
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K. Maguire, J. Thompson, and S. Gowland Dinantian depositional environments along the northern margin of the Solway Basin, UK Geological Society, London, Special Publications, 1996; 107: 163 - 182. [Abstract] [PDF] |
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M. K. LEE A new gravity survey of the Lake District and three-dimensional model of the granite batholith Journal of the Geological Society, 1986; 143: 425 - 435. [Abstract] [PDF] |
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