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Geology and geochronology of McMurdo Volcanic Group rocks in the vicinity of Lake Morning, McMurdo Sound, Antarctica

机译:南极麦克默多峡湾晨湖附近的麦克默多火山群岩石的地质和年代学

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Trachyandesite lava flows and trachytic dykes exposed at ‘Gandalf Ridge’ and near Lake Morning on the northern slopes of Mount Morning represent the oldest exposed volcanic rocks in the Erebus volcanic province of the McMurdo Volcanic Group. Conventional whole rock K-Ar age determinations show the rocks are mid-Miocene, ranging between 14.6 and 18.7 Ma. North–south trending faults, which parallel the Transantarctic Mountains, cut the dated dykes. The faults are probably part of a broad fault zone which bounds the uplifted Transantarctic Mountains and the down-dropped Ross Sea/Ross Ice Shelf embayment.
机译:在“甘道夫岭”和早晨山北坡的早晨湖附近暴露的菱锰矿熔岩流和菱形堤坝是麦克默多火山群的埃里布斯火山省中最古老的裸露火山岩。传统的整体岩石K-Ar年龄测定表明,这些岩石是中新世中期,范围在14.6和18.7 Ma之间。与跨南极山脉平行的南北向断层切断了过时的堤防。这些断层可能是一个宽泛的断层带的一部分,该断层带限定了隆起的南极山脉和下降的罗斯海/罗斯冰架通道。

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