The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

生贴的力士柄嵌者应是俗称之杂石，并非红、绿宝石。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武绿柱石宝石晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是俗称之杂，并非红、绿宝。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和、、气成—热液条件下形成的四川平武绿柱宝晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是杂，并非红、绿。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武绿柱晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是俗称之杂石，并非红、宝石。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平石宝石晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是杂，并非红、绿。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武绿柱晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是俗称之杂石，并非红、绿宝石。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武绿柱石宝石晶,有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的柄嵌者应是俗称之杂，并非红、绿宝。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武绿柱宝晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是俗称之杂石，并非红、石。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、—液条件下形的四川平武柱石石晶体,具有特征的扁平板状几何外形。

The stone on hilt of keris posted by Mr.Wudao should be the so-called farraginous stone,not the ruby or beryl.

无刀先生贴的克力士柄嵌者应是俗称之杂，并非红、。

The beryl crystal from Pingwu County,Sichuan Province that occurred on the low saturation,alkaline and pneumatogenic—thermal conditions,is characterized by the flat tabular shape.

在低饱和度、碱性、气成—热液条件下形成的四川平武柱晶体,具有特征的扁平板外形。