ISSN 1000-3665 CN 11-2202/P

    云南省安宁温泉地热地质特征及成因模式

    Characteristics of geothermal geology and genetic model of the Anning hot spring in Yunnan Province

    • 摘要: 安宁温泉为上升泉群,其热水化学类型为HCO3—Ca.Mg和HCO3—Ca型。泉群地温场平面特征是在"天下第一汤"形成高温中心,垂向上则随深度变化井温曲线呈现增温型、恒温型、增降骤变型和增温变降温型四种类型。热储具多元结构,当前利用热水除温泉自流水量外都取自浅部热储。温泉流量与降雨补给关系密切,热储具有开放式特征,热水循环周期在21a以上。安宁温泉的热源来自区域高热流背景,螳螂川断裂起到导热导水作用,其成因模式为大气降水补给的断裂深循环型地热系统。

       

      Abstract: The Anning hot spring,reputed as "the most wonderful hot spring in the world", is an ascending spring group.The hydrochemical type of the thermal water is HCO3—Ca·Mg or HCO3—Ca type.Horizontally,the geothermal field is characterized by a high temperature center at "the most wonderful hot spring in the world".In the vertical direction the characteristics change with depth.The welltemperature curves can be grouped into four types,i.e.,the temperature-increasing type,the constant-temperature type,the suddenly increasing-decreasing type and the temperature-increasing-temperature-decreasing type.The thermal reservoirs are composed of multivariate structures.The currently-used thermal water originates from some superficial thermal reservoirs.The discharge of the hot spring is closely related to supply of rainfall,being an open supply pattern.The circulation period of thermal water is over 21 years.The analysis results show that heat source of the Anning hot spring originates from the regional high heat flow background and its water resource from atmospheric precipitation.The Tanglangchuan fault is a passage through which water and heat transmit.Therefore, the geological genetic model of the Anning hot spring is a deep-fault circulation geothermal system with an open supply pattern.

       

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