They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些床可分为高硫低硫,且都具有典的围岩蚀变、蚀变分带等床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切带内造岩、围岩蚀变分带明显,并具有典的“(超)糜棱岩—石英、黄铁、铁白云石—”等“三位一体”成特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎带的岩石具有明显的对称分带性：破碎带的中心为钠柱石体，向两侧依次为榍石透辉石长英岩带、黑云母钠长岩带，并逐渐过渡为围岩。钠柱石的成因类为沿造破碎带产出的热液交代脉。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

床可分为高硫化型和低硫化型,且都具有典型的围岩蚀变、蚀变分带等床。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切带内造岩、围岩蚀变分带明显,并具有典型的“(超)糜棱岩—石英、黄铁、铁白云石化—金化”等“三位一体”成。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎带的岩石具有明显的对称分带性：破碎带的中心为钠柱石体，向两侧依次为榍石透辉石长英岩带、黑云母钠长岩带，并逐渐过渡为围岩。钠柱石的成因类型为沿造破碎带产出的热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可为高硫化型和低硫化型,且都具有典型的围岩蚀变、蚀变等矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧剪切内造岩、围岩蚀变明显,并具有典型的“(超)糜棱岩—石英、黄铁矿、铁白云石化—金矿化”等“三位一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎的岩石具有明显的对称：破碎的中心为钠柱石矿体，向两侧依次为榍石透辉石长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱石矿的成因类型为沿造破碎产出的热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可分化型和低化型,且都具有典型的围岩蚀变、蚀变分带矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切带内造岩、围岩蚀变分带明显,并具有典型的“(超)糜棱岩—石英、黄铁矿、铁白云石化—金矿化”“一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎带的岩石具有明显的对称分带性：破碎带的中心钠柱石矿体，向两侧依次榍石透辉石长英岩带、黑云母钠长岩带，并逐渐过渡围岩。钠柱石矿的成因类型沿造破碎带产出的热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可分为高硫化型和低硫化型,且都具有典型围蚀变、蚀变分等矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切内造、围蚀变分明显,并具有典型“(超)糜棱—石英、黄铁矿、铁白云石化—金矿化”等“三位一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎石具有明显对称分性：破碎中心为钠柱石矿体，向两侧依次为榍石透辉石长英、黑云母钠长，并逐渐过渡为围。钠柱石矿成因类型为沿造破碎产出热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可分为高硫化型和低硫化型,且都具有典型围岩蚀变、蚀变分等矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切内造岩、围岩蚀变分明显,并具有典型“(超)糜棱岩—石英、黄铁矿、铁白云石化—金矿化”等“三位一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎岩石具有明显对称分性：破碎心为钠柱石矿体，向两侧依次为榍石透辉石长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱石矿成因类型为沿造破碎产出热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可为高硫化型和低硫化型,且都有典型的围岩蚀、蚀等矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切内造岩、围岩蚀明显,并有典型的“(超)糜棱岩—石英、黄铁矿、铁白云石化—金矿化”等“三位一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎的岩石有明显的对称性：破碎的中心为钠柱石矿体，向两侧依次为榍石透辉石长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱石矿的成因类型为沿造破碎产出的热液交代脉型。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些矿床可分为高硫化和低硫化,且都具有典围岩、分带等矿床特征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切带内造岩、围岩分带明显,并具有典“()糜棱岩—石英、黄铁矿、铁白云石化—金矿化”等“三位一体”成矿特征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎带岩石具有明显对称分带性：破碎带中心为钠柱石矿体，向两侧依次为榍石透辉石长英岩带、黑云母钠长岩带，并逐渐过渡为围岩。钠柱石矿成因类为沿造破碎带产出热液交代脉。

They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.

这些可分为高硫化型和低硫化型,且都具有典型的围岩蚀变、蚀变分等征。

In the ductile shear belt,the alteration and zonation of tectonite and wall rock are obviously,and miliolite belt,quartz,iron pyrite,ankerite alteration belt and gold mineralization belt are trinity.

韧性剪切内造岩、围岩蚀变分,并具有典型的“(超)糜棱岩—石英、黄铁、铁白云石化—金化”等“三位一体”成征。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

造破碎的岩石具有的对称分性：破碎的中心为钠柱石体，向两侧依次为榍石透辉石长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱石的成因类型为沿造破碎产出的热液交代脉型。