The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括安岩、安岩、钠长岩以及角砾岩、凝灰岩等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石岩带主要为层状，产于泥盆系星红铺组粉岩中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑岩亚类岩石类型主要为安熔结集块岩,安、英安及流纹火角砾岩以及流纹熔结凝灰岩。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

单元不仅仅由玄武组成，还包括安山、安、以及角砾、凝灰等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含石带主要为层状，产于泥盆系星红铺组粉砂质板中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑亚类石类型主要为安山质熔结集块,安山质、英安质及流纹质火山角砾以及流纹质熔结凝灰。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括安山、安、钠长以及角砾、凝等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长带主要为层状，产于泥盆系星红铺组粉砂质板中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常山碎屑亚主要为安山质熔结集块,安山质、英安质及流纹质山角砾以及流纹质熔结凝。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括、、钠长以及角砾、凝灰等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石带主要为层状，产于泥盆系星红铺组粉板中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑亚类石类型主要为熔结集块,、英及流纹火角砾以及流纹熔结凝灰。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

积金矿床的矿体是一些不连续的内生或后生地体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩成，还包括安山岩、安岩、钠长岩以及角砾岩、凝灰岩等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石岩带主要为层状，产于泥盆铺粉砂质板岩中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑岩亚类岩石类型主要为安山质熔结集块岩,安山质、英安质及流纹质火山角砾岩以及流纹质熔结凝灰岩。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括、、钠长以及角砾、凝灰等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石带主要为层状，产于泥盆系星红铺组粉砂质板中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑亚类石类型主要为质熔结集块,质、英质及流纹质火角砾以及流纹质熔结凝灰。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩成，还包括安山岩、安岩、钠长岩以及角砾岩、凝灰岩等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石岩带主要为层状，产于泥盆系星红砂板岩中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火山碎屑岩亚类岩石类型主要为安山熔结集块岩,安山、英安及流纹火山角砾岩以及流纹熔结凝灰岩。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床矿体是一些不连续内生或后生地体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括安岩、安岩、钠长岩以及角砾岩、凝灰岩等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石岩带主要为层状，产于泥盆系星红铺组粉岩中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑岩亚类岩石类型主要为安熔结集块岩,安、英安及流纹火角砾岩以及流纹熔结凝灰岩。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括安、安、钠长以及角砾、凝灰等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石带主要为层状，产于泥盆系星红铺组粉板中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常火碎屑亚类石类型主要为安结集块,安、英安及流纹火角砾以及流纹结凝灰。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出单元不仅仅由玄武组成，还包括安、安、钠长以及角砾、凝灰等。

The Shuangwang gold-bearing albitite zone, which is composed of stratabound albitite, albitite breccia occurred conformably in the Xinghongpu Group, Devonian silt-slate.

双王含金钠长石带主要为层状，产于泥盆系星红铺组粉砂中。

The first rock is mainly andesite clinkering agglomerate, andesite breccia, dacite breccia, rhyolite breccia and rhyolite clinkering tuff.

正常碎屑亚类石类型主要为安熔结集块,安、英安及流纹角砾以及流纹熔结凝灰。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内生或后生地体,通常赋存于断裂带、角砾体或层(性单位)中。

The dissolved pore and intercrystal pore are the most important reservoir spaces. followed by breccias. and dissolved breccia pores. and the moldic and fenestral pores are less important.

就其储集意义而言，以溶孔和晶间孔最为重要，次为角砾孔及砾间溶孔，而铸模孔和窗格孔的储集意义相对次要。