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Geology of Lizard, Cornwall : ウィキペディア英語版
Lizard complex

The Lizard Complex, Cornwall is a preserved example of an exposed ophiolite complex in the United Kingdom. The rocks found in The Lizard area are analogous to those found in such famous areas as the Troodos Mountains, Cyprus and the Semail Ophiolite, Oman.
==Lithologies==
The Lizard comprises three main units; the serpentinites, the 'oceanic complex' and the metamorphic basement. Since the pioneering work of Bromley〔Bromley, A.V. (1975). Is the Lizard Complex, South Cornwall, a fragment of Hercynian oceanic crust?. The Lizard: A Magazine of Field Studies, 5:3, pp. 2–11.〕〔Bromley, A.V. (1976). A new interpretation of the Lizard Complex, S. Cornwall, in the light of the ocean crust model. Proc. Geol. Soc. London, 132, p. 114.〕 and Kirby〔Kirby, G. A. (1979). The Lizard Complex as an ophiolite. Nature, London, 282, pp. 58–61.〕 these suites have been understood to represent a slice through a section of ocean crust, including the upper level of the mantle, thrust onto continental crust.

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