The northwest Guangxi belongs to the rift zone of Dian ( Yunnan ) - Qian ( Guizhou ) - Gui ( Guangxi ) with a high geothermal field.

桂西北地区属滇 黔 桂裂谷,具高的地热场环境.

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Basin basement palaeo - heat flow is a basic boundary parameter condition to realize basin geothermal field simulation.

盆地基底古热流是实现盆地地热场模拟的基础边界参数条件.

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It will provide a scientific basis for the rational exploitation and utilization of the geothermal field.

在此基础上提出该地下热水系统的成因模式,为地热田的进一步合理开发利用提供了依据.

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