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Wetterstein dolomite : ウィキペディア英語版 | Wetterstein limestone
Wetterstein limestone ((ドイツ語:Wettersteinkalk)) and Wetterstein dolomite (''Wettersteindolomit'') are the most common names for a carbonate rock from the Middle Triassic epoch of the Ladinian stage, comparable to the German stage in which Muschelkalk rock strata were formed. The rock gets its name from the Wetterstein Mountains, because the Wetterstein limestone is the bedrock of large mountains here. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians. ==Geology==
The rock is found in the whole of the Alps, in many places as limestone (calcium carbonate), in many others as dolomite. In many areas there is a frequent alternation of limestone and dolomite facies.
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「Wetterstein limestone」の詳細全文を読む
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