It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩浆演化序列中所处位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成矿物质源于碱性武岩浆，基性次火山岩浆多次脉动式入侵是矿床形成必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

矿床类型以岩浆晚期分异交代型、气成热液型、伟晶岩型、风化壳型和砂矿型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩测矿物有捕虏成因、岩浆成因、地幔成因等各种来源时，可分别求出某单一事件年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

元在岩浆演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成矿物质源于碱性武岩浆，基性次火山岩浆多次脉动式入侵是矿床形成的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

矿床类型以岩浆晚期分异交代型、气成热液型、伟晶岩型、风化壳型和砂矿型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因，些岩体的被测矿物有捕虏体成因、岩浆成因、地幔成因等各种来源时，可分别求出一事件的年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗液态不混溶作用也是伟晶成成矿的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成矿物质性武，性次火山多次脉动式入侵是矿床形成的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

矿床类型以晚期分异交代型、气成热液型、伟晶型、风化壳型和砂矿型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些体的被测矿物有捕虏体成因、成因、地幔成因等各种来时，可分别求出某单一事件的年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩浆演化序列中所处位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模外,富氟花岗岩浆液态不混溶作用也是伟晶岩岩重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

物质源于碱性武岩浆，基性次火山岩浆多次入侵是床形必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

床类型以岩浆晚期分异交代型、气热液型、伟晶岩型、风化壳型和砂型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩体被测物有捕虏体因、岩浆因、地幔因等各种来源时，可分别求出某单一事件年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式,花岗岩液态不混溶作用也是伟晶岩成岩成矿的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成矿物质源于碱性武岩，基性次火山岩多次脉动式入侵是矿床形成的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

矿床类型以岩分异交代型、气成热液型、伟晶岩型、风化壳型和砂矿型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩体的被测矿物有捕虏体成因、岩成因、地幔成因等各种来源时，可分别求出某单一事件的年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩浆演化序列中所处位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成物质源于碱性武岩浆，基性次火山岩浆多次脉动式入侵是床形成必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

床类型以岩浆晚期分异交代型、气成热液型、伟晶岩型、风化壳型和砂型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩体物有捕虏体成因、岩浆成因、地幔成因等各种来源时，可分别求出某单一事件年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗岩不混溶作用也是伟晶岩成岩成的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成物质源于碱性武岩，基性次火山岩多次脉动式入侵是形成的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

型以岩晚期分异交代型、气成热型、伟晶岩型、风化壳型和砂型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩体的被测物有捕虏体成因、岩成因、地幔成因等各种来源时，可分别求出某单一事件的年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在岩浆演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模式外,富氟花岗岩浆混溶作用也是伟晶岩成岩成的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

成物质源于碱性武岩浆，基性次火山岩浆多次脉动式入侵是形成的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

类型以岩浆晚期分异交代型、气成热型、伟晶岩型、风化壳型和砂型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些岩体的被测物有捕虏体成因、岩浆成因、地幔成因等各种来源时，可分别求出某单一事件的年龄。

It's difficult to decide the position of the unit in evolutional seriary of magma.

该单元在浆演化序列中所处的位1难以确定。

Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.

除了结晶分异模外,富氟花岗浆液态不混溶作用也是伟晶矿的重要机制。

The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.

矿物质源于碱性武浆，基性次火山浆多次脉动是矿床形的必要条件。

The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.

矿床类型以浆晚期分异交代型、气热液型、伟晶型、风化壳型和砂矿型为主。

Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.

因此，当某些体的被测矿物有捕虏体因、浆因、地幔因等各种来源时，可分别求出某单一事件的年龄。