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・ Moinabad, Razavi Khorasan
・ Moinabad, Sanandaj
・ Moinabad, Semnan
・ Moinabad, South Khorasan
・ Moinabad, Tehran
・ Moinabad-e Bala
・ Moinabad-e Sofla
・ Moinak Hydro Power Plant
・ Moinatrindri
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・ Moindah River
・ Moindou
・ Moindou Bay
・ Moindou River
・ Moine
Moine Supergroup
・ Moine Thrust Belt
・ Moineau
・ Moineaux de Paris
・ Moinee Foundation
・ Moineville
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・ Moingi language
・ Moingona
・ Moingona, Iowa
・ Moings
・ Moinho de Maré de Corroios
・ Moinhos de Vento
・ Moinhos de Vento Park
・ Moinidae


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Moine Supergroup : ウィキペディア英語版
Moine Supergroup

The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks that form the dominant outcrop of the Scottish Highlands between the Moine Thrust Belt to the northwest and the Great Glen Fault to the southeast. The sequence is metasedimentary in nature and was metamorphosed and deformed in a series of tectonic events during the Late Proterozoic and Early Paleozoic. It takes its name from ''A' Mhòine'', a peat bog in northern Sutherland.
==Distribution==
The main outcrop of the Moine series lies northwest of the Great Glen Fault, structurally above the Moine Thrust to the west forming what is known as the Northern Highlands Terrane.〔(Strachan, R.A., Smith, M., Harris, A.L.& Fettes, D.J. 2002. Chapter 4: The Northern Highland and Grampian terranes in: Trewin, N.H (Ed) The Geology of Scotland, Geological Society, London, 550pp. )〕 A smaller area of similar rocks that are correlated with these, outcrop within the 'Grampian Terrane' to the southeast of the Great Glen. Moinian rocks are also recognised on Mull, Orkney and Shetland.

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