1.These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.
结果表明,该地区全新世大暖期
古土壤为温湿气候条件
溶褐土,并非过去所称半干旱条件“黑垆土”.
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