过:真品红山玉的“过”渡.必须注重其在土中的埋藏方位,处于土层最下端水浸蚀时间最长,故其质变最严重《玉软沁方入》,呈减缩态.质变与色变向上依次渐变呈包裹状。并少数<font face="Verdana">在</font><font face="Verdana">方<font face="Verdana">位</font><font face="Verdana">下<font face="Verdana">端</font><font face="Verdana">质<font face="Verdana">变</font><font face="Verdana">处</font></font></font></font>伴有腐蚀质有机炭沁入《多呈周身同状态开口且边口色清晰》和硬质解理显现..而老料带沁仿品,无对应内外质变的方位感 ,观其表层沁蚀程度与内质质变不对应,表象的色和质变非渐变包裹状。[upload=jpg,20080227_3dbd8d0a645f28887101kca6k48hgrxp.jpg]UploadFile/2008-6/20086110431958879.jpg[/upload]<br/>[upload=jpg,20080227_3fea5e977934525b6039la5tm89gk6dk.jpg]UploadFile/2008-6/20086110431951421.jpg[/upload]<br/>
[此贴子已经被作者于2008-6-1 10:43:26编辑过]
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