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
构造运动、全
平面变化等具有重要
科研、科普价值。
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前;纪元;;;;;;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.
对于研究全构造运动、全平面变化等具有重要科研、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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