《Table 3 Weathering indices and density of the collected samples》
![《Table 3 Weathering indices and density of the collected samples》](http://bookimg.mtoou.info/tubiao/gif/SDKB201903001_21000.gif)
本系列图表出处文件名:随高清版一同展现
《"Origin of the Mushroom Stone Forest at the southeastern foot of the Little Sangpu Mountain in eastern Guangdong,China: A palaeo-sea-level indicator or not"》
Notes:R=Ruxton Ratio;CIA=Chemical Index of Alteration;WIP=Weathering Index of Parker;LOI=Loss on ignition.
The weathering debris(MLH-T2)has the lowest density with an average value of 2.32,followed by the density of the the cutting surface(MLH-T3),whose average value is 2.36.The concavity apex of the boulder(MLH-T1)has the third lowest density with an average value of 2.43.The average density values of the rock samples taken from the top(MLH-D3)and the concavity roof(MLH-S2)of the boulder are 2.45 and 2.46,respectively.The density of the fresh rock sample(MLH-X2)has the highest value with an average of2.64.The density’values are listed in Table 3.
图表编号 | XD0056559900 严禁用于非法目的 |
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绘制时间 | 2019.03.01 |
作者 | LI Jian-cheng、WANG Wei、ZHENG Yan-ming |
绘制单位 | Geography department of Hanshan Normal University、Geographic school of South China Normal University、Geography department of Hanshan Normal University |
更多格式 | 高清、无水印(增值服务) |
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