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Beacon sandstone : ウィキペディア英語版 | Beacon Supergroup
The Beacon Supergroup is a geological formation exposed in Antarctica and deposited from the Devonian to the Triassic (). The unit was originally described as either a formation or sandstone, and upgraded to group and supergroup as time passed. It contains a sandy member known as the Beacon heights orthoquartzite. 〔(Bradshaw, M. (2013, August 6) The Taylor Group (Beacon Supergroup): the Devonian sediments of Antarctica ), Geological Society (81), 67-97. Accessed December 13, 2013.〕 ==Setting in time and space== Named after Beacon Heights. First named 1907, type section described in 1963. Originally dubbed a formation, with scope left (and later used) to expand to group, then supergroup, as better mapped and understood.〔
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「Beacon Supergroup」の詳細全文を読む
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