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用质变料仿制 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]UploadFile/2008-5/20085111243142837.jpg[/upload] [upload=jpg]UploadFile/2008-5/20085111243135380.jpg[/upload] [upload=jpg]UploadFile/2008-5/20085111243115556.jpg[/upload] [upload=jpg]UploadFile/2008-5/20085111243134300.jpg[/upload] [upload=jpg]UploadFile/2008-5/20085111243123202.jpg[/upload]
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