穆特诺夫斯基地热矿床属于硫质热液喷气型,类似于加利福尼亚的盖捷尔斯(Γейэерс)、日本的玛楚卡瓦(Мацукава)、堪察加的下科舍列夫斯基(Нижнекошелевский)等地热矿床。该矿床的天然热液露头为沸腾的硫化铵热泉和蒸汽流,形成于硫质喷气田内。钻探结果表明,在深部蒸气相很丰富;因此,这类热液系统称为以蒸汽为主的热液系统。在与此成鲜明对照的系统——以高温热水为主的系统(通 The Muthernovsky geothermal deposit belongs to the pyritic hydrothermal jet, similar to the Géjérguez in California, the Мацукава in Japan, the Kokoshevsky in Kamchatka Нижнекошелевский) and other geothermal deposits. The natural hydrothermal outcrop of this deposit is a boiling ammonium sulphide hot spring and steam stream formed in a sulfur-rich gas field. Drilling results show that the vapor phase is abundant in the deep; therefore, this type of hydrothermal system is referred to as a steam-based hydrothermal system. In sharp contrast with this system - hot water system (pass