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Central Highlands Terrane : ウィキペディア英語版 | Central Highlands Terrane The Central Highlands Terrane, also known as the Grampian Terrane, is a sequence of early Paleozoic metamorphic rocks containing many igneous intrusions. It stretches from the Great Glen Fault, south-east down to the Highland Boundary. The terrane contains mostly gabbro and gneiss that show intrusions of granite and dolerite. Limestones in the region also contain many fossils such as trilobites and brachiopods.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Central Highlands Terrane」の詳細全文を読む
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