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Mud and fluid migration in active mud volcanoes in Azerbaijan

机译:阿塞拜疆活跃泥火山中的泥浆和流体迁移

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Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed. [References: 60]
机译:阿塞拜疆的泥火山喷发通常持续不到几个小时,其特征是泥砾角砾岩,烃类气体和水的剧烈挤压。最近的实地调查和对四个活泼泥火山的测绘表明,休眠期的活动范围从泥浆和流体的静流到剧烈流动。排出水的地球化学分析显示,溶质浓度范围很广,表明存在复杂的管道系统。泥浆和流体起源很深,但有时会存储在中等深度的泥浆室中。提出了深层咸水与浅层大气之间的混合模型。 [参考:60]

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