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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Geochemical constraints for the origin of thermal waters from western Turkey [Review]
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Geochemical constraints for the origin of thermal waters from western Turkey [Review]

机译:土耳其西部温泉水起源的地球化学限制因素[综述]

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The combined chemical composition, B and Sr isotopes, and the basic geologic setting of geothermal systems from the Menderes Massif in western Turkey have been investigated to evaluate the origin of the dissolved constituents and mechanisms of water-rock interaction. Four types of thermal water are present: (1) a Na-Cl of marine origin; (2) a Na-HCO3 type with high CO2 content that is associated with metamorphic rocks of the Menderes Massif; (3) a Na-SO4 type that is also associated with metamorphic rocks of the Menderes Massif with H2S addition; and (4) a Ca-Mg-HCO3-SO4 type that results from interactions with carbonate rocks at shallow depths. The Na-Cl waters are further subdivided based on Br/Cl ratios. Water from the Cumali Seferihisar and Bodrum Karaada systems are deep circulated seawater (Br/Cl=sea water) whereas water from Canakkale-Tuzla (Br/Cl < sea water) are from dissolution of Messinian evaporites. Good correlations between different dissolved salts and temperature indicate that the chemical composition of the thermal waters from non-marine geothermal systems is controlled by: (1) temperature dependent water-rock interactions; (2) intensification of reactions due to high dissolved CO2 and possibly HCl gasses; and (3) mixing with overlying cold groundwater. All of the thermal water is enriched in B. The B isotopic composition (delta(11)B=2.3parts per thousand to 18.7parts per thousand; n=6) can indicate either leaching of B from the rocks, or B(OH)(3) degassing flux from deep sources. The large ranges in B concentrations in different rock types as well as in thermal waters from different systems suggest the water-rock mechanism. Sr-87/Sr-86 ratios of the thermal water are used to differentiate between solutes that have interacted with metamorphic rocks (Sr-87/Sr-86 ratio as high as 0.719479) and carbonate rocks (low Sr-87/Sr-86 ratio of 0.707864). (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 101]
机译:研究了组合化学成分,B和Sr同位素以及土耳其西部Menderes Massif地热系统的基本地质环境,以评估溶解成分的起源和水-岩相互作用的机理。存在四种类型的热水:(1)海洋来源的Na-Cl; (2)具有高CO2含量的Na-HCO3型,与Menderes地块的变质岩有关; (3)Na-SO4类型,也与添加了H2S的Menderes地块的变质岩有关; (4)一种Ca-Mg-HCO3-SO4类型,是由于与浅层碳酸盐岩相互作用而产生的。根据Br / Cl比例进一步细分Na-Cl水。来自Cumali Seferihisar和Bodrum Karaada系统的水是深循环海水(Br / Cl =海水),而来自Canakkale-Tuzla的水(Br / Cl <海水)则来自于墨西尼蒸发岩的溶解。不同溶解盐和温度之间的良好相关性表明,来自非海洋地热系统的热水的化学成分受以下因素控制:(1)温度相关的水-岩相互作用; (2)由于高溶解的二氧化碳和可能的HCl气体而引起的反应加剧; (3)与上覆的冷地下水混合。所有的热水都富含B。B的同位素组成(δ(11)B =每千份中有2.3份至每千份中有18.7份; n = 6)可以表明从岩石中浸出了B或B(OH) (3)从深处除气。不同岩石类型以及来自不同系统的热水中B浓度的变化幅度很大,表明水岩石机制。 Sr-87 / Sr-86比值的热水用于区分与变质岩相互作用的溶质(Sr-87 / Sr-86比值高达0.719479)和碳酸盐岩(低Sr-87 / Sr-86)比为0.707864)。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:101]

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