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About this book
Yell is a sparsely populated island in the north of Shetland, and is separated from neighbouring Unst and Mainland by two faults. Its geology has been little studied until now.
Contents
Structural and stratigraphical succession; Lewisian inliers; metasedimentary rocks; early igneous rocks; gneisses and gneissification; structures; Hascosay slide; late intrusive rocks; radiometric ages; geophysics; Pleistocene and recent; stream sediment geochemistry; economic geology.
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