Wuguan marine erosion physiognomy has important geognosy significance in the study of structural movement and the changes in sea level in period of Holocene Epoch.
对于研究全新世构造运动、全新世海平面变
有重要
科研、科普价值。
；全新世
),全新统()
;;;;;;河;;;Wuguan marine erosion physiognomy has important geognosy significance in the study of structural movement and the changes in sea level in period of Holocene Epoch.
对于研究全新世构造运动、全新世海平面变有重要科研、科普价值。
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下发育淋溶褐土,并非过去所称半干旱条件下发育“黑垆土”.
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