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、全新世海平面变化等具有重要的科研、科普价值。
生的;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、全新世海平面变化等具有重要的科研、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的古土壤为温湿气候条件
的淋溶褐土,并非过去所称的半干旱条件的“黑垆土”.
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