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Widgiemooltha Komatiite
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Widgiemooltha Komatiite : ウィキペディア英語版
Widgiemooltha Komatiite
The Widgiemooltha Komatiite is a formation of komatiite in the Yilgarn Craton of Western Australia.
== Stratigraphy ==
The stratigraphy of the Widgiemooltha Komatiite is well known to be part of the regional komatiite magmatic event also seen at the Kambalda Dome, to the north. There are comparisons which place the Widgiemooltha Komatiite as equivalent to the Silver Lake Komatiite. The Mt Edwards Basalt is correlated regionally with the Devon Consuls Basalt of Kambalda, and the Widgeimooltha Chert correlated with the Paringa Slate.
The structure of the Widgiemooltha Dome has three thrusted repetitions of the basal komatiite contact and komatiite sequence including footwall Mt Edwards Basalt and hangingwall sediments (Widgiemooltha Chert).

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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