Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金的成矿活动有关的硅化、粘土化蚀变是黑刺沟金矿金矿床在的地。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化菌的生长;中、碱性条件下,氨化菌仍能维持正常生长;苏州河的氨化菌无法以无机氮和尿素作为生长所需的氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与的成活动有关的硅化、粘土化蚀变是黑刺沟规模床在的地质前。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

表明,低温、高盐度和酸性条件会抑制氨化菌的生长;中、碱性条件下,氨化菌仍能维持正常生长;苏州河的氨化菌无法以无机氮和尿素作为生长所需的氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金成矿活动有关硅化、粘土化蚀变是黑刺沟金矿田规模金矿床在地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化菌生长;中、碱性条件下,氨化菌仍能维持正常生长;苏氨化菌无法以无机氮和尿素作为生长所需氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

偏碱性花岗岩及与金的成矿活动有关的硅、粘土蚀变是黑刺沟金矿田规模金矿床在的地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨的生长;中、碱性条件下,氨能维持正常生长;苏州河的氨无法以无机氮和尿素作为生长所需的氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金成矿活动有关硅化、粘土化蚀变是黑刺沟金矿田规模金矿床在地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化菌生长;中、碱性条件下,氨化菌仍能维持正常生长;苏氨化菌无法以无机氮和尿素作为生长所需氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

要偏碱性花岗岩及与金的成矿活动有关的硅化、粘土化蚀变是黑刺沟金矿田规模金矿床在的地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化的生长;中、碱性条件下,氨化维持正常生长;苏州河的氨化无法以无机氮和尿素作为生长所需的氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金成矿活动有关硅化、粘土化蚀变是黑刺沟金矿田规模金矿床在地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化菌生长;中、碱性条件下,氨化菌仍能维持正常生长;苏州河氨化菌法机氮和尿素作为生长所需氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金的成矿活动有关的硅、蚀变是黑刺沟金矿田规模金矿床在的地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐性条件会抑制氨菌的生长;中、碱性条件下,氨菌仍能维持正常生长;苏州河的氨菌无法以无机氮尿素作为生长所需的氮源;

Alkalescent granites and gold-related silication and argillation are geological prerequisites for the formation of noticeable gold deposits.

摘要偏碱性花岗岩及与金成矿活动有关硅化、粘土化蚀变是黑刺沟金矿田规模金矿床在地质前提。

The results showed that low temperature, high content of salt and acidic condition inhibited ammonifiers growth, and alkalescent condition showed little effect on ammonifiers.

结果表明,低温、高盐度和酸性条件会抑制氨化菌生长;中、碱性条件下,氨化菌仍能维持正常生长;苏州河氨化菌无法以无机氮和尿素作为生长所氮源;