Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

金属矿是一个老矿山,它产于—杨杖岩浆热液成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含金属硫物的钨锰-白钨矿矿床会产主一系列的物理、，形成次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八金属矿是一个老矿山,它产于八—杨岩浆热液成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含金属硫化钨锰-白钨矿矿床会产主一系列、化学变化，形成次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子金属矿是个老矿山,它产于八家子—杨家杖子岩成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含金属硫化物的钨锰-白钨矿矿床会产列的物理、化学变化，形成次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子金属是一个老山,它于八家子—杨家杖子岩浆热带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含金属硫化物的钨锰-白钨床一系列的物理、化学变化，形次生富集钨床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子金属矿是一个老矿山,它产于八家子—杨家杖子岩浆热液成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气件下，含金属的钨锰-白钨矿矿床会产主一系列的理、学变，形成次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子是一个老山,它产于八家子—杨家杖子岩浆热液成带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含硫化物的钨锰-白钨床会产主一系列的物理、化学变化，形成次生富集钨床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子属矿是一个老矿山,它产于八家子—杨家杖子岩浆热液成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含属硫化物的钨锰-白钨矿矿床会产主一系列的物理、化学变化，形成次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子金属矿是一个老矿山,它产于八家子—杨家杖子岩浆热液矿带南西。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件下，含金属硫化物的钨锰-白钨矿矿床会产主一系列的物理、化学变化，形次生富集钨矿床。

Bajiazi polymetallic ore deposit is an old mine,which occured in southeastern part of Bajiazi-Yangjiazhangzi magmatic hydrotherm metallogenic belt.

八家子矿是一个老矿山,它产于八家子—杨家杖子岩浆热液成矿带南西部。

Under hygrothermal climate, a series of physicochemical changes take place on huebnerite-scheelite deposit,containing polymetallic sulphi-des and slich a deposit forms a secondary tungsten deposit.

在温湿气候条件，化物的钨锰-白钨矿矿床会产主一系列的物理、化学变化，形成次生富集钨矿床。