Drill cores of Miocene rocks in Brazil, which provided the only complete sequence of the change from reddish clays to the blue and brown sediments, further corroborated my conclusions.
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巴西的中新世岩石钻探岩心,提供了淡红色黏土连续转变成蓝棕色沉积物的证据,更加支持了我的结论。
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