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首页> 外文期刊>Geothermics >Curie point depth, heat-flow and radiogenic heat production deduced from the spectral analysis of the aeromagnetic data for geothermal investigation on the Menderes Massif and the Aegean Region, western Turkey
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Curie point depth, heat-flow and radiogenic heat production deduced from the spectral analysis of the aeromagnetic data for geothermal investigation on the Menderes Massif and the Aegean Region, western Turkey

机译:从航空磁数据的频谱分析得出的居里点深度,热流和放射性热产生,用于土耳其西部Menderes地块和爱琴海地区的地热研究

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In this study, the Curie point depth (CPD), heat-flow and radiogenic heat production maps of the Menderes Massif (MM) and the Aegean Region-Turkey were prepared for the thermal crustal structure from the aeromagnetic data by means of a spectral analysis method. The estimated CPDs in the study area vary from 6.21 to 12.41 km. The heat-flow values were calculated for two (2) different thermal conductivities of 2.5-2.7 Wm(-1) K-1. The radiogenic heat production was also calculated between 0.38 and 0.80 mu W m(-3) on the high-grade metamorphic units of the study area. The estimated heat-flow and radiogenic heat production maps indicate that a high temperature in the upper crust and thin lithosphere in the observation area are probably resulted from the crustal extension, active deformation and magmatism. All of the produced maps in this study were correlated with the analytic signal (AS) map which indicates the locations of the bodies causing magnetic anomalies. In addition, maxspots of the horizontal gradients from the magnetic anomalies were also emplaced onto the produced maps to indicate the boundaries of critical magmatic units in the study area. These correlations allow reasonable and meaningful interpretation for the reasons of high geothermal gradient and high heat-flow. In addition, a longitudinal seismic wave (V-p velocity) map was presented from the relationship between seismic velocity and radiogenic heat production in the western Anatolia, for the first time and they were correlated with the previous investigations. The estimated V-p velocities range from about 6 to 6.4 km/sn and low V-p values may be related to the partial melting of subducted structures in the western Anatolia. As a result, two new potential geothermal areas were determined by the integration of different methods used in this study. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在这项研究中,通过光谱分析从航空磁数据中为热地壳结构绘制了Menderes地块(MM)和爱琴海地区土耳其的居里点深度(CPD),热流和放射致热图。方法。研究区域的估计CPD范围从6.21到12.41 km。针对两(2)个2.5-2.7 Wm(-1)K-1的不同热导率计算了热流值。在研究区域的高级变质单元上,还计算出了辐射热产生量在0.38至0.80μW m(-3)之间。估计的热流图和放射致热图表明,观测区上地壳和薄岩石圈的高温可能是由于地壳伸展,活动变形和岩浆作用造成的。这项研究中产生的所有图都与分析信号(AS)图相关,该图指示了引起磁异常的物体的位置。此外,还将来自磁异常的水平梯度的最大点放置在生成的图上,以指示研究区域中关键岩浆单元的边界。由于高地热梯度和高热流的原因,这些相关性允许合理且有意义的解释。此外,首次从地震速度与安那托利亚西部放射源热产生之间的关系绘制了纵向地震波(V-p速度)图,并将其与先前的研究相关联。估计的V-p速度范围约为6至6.4 km / sn,低的V-p值可能与安纳托利亚西部俯冲结构的部分融化有关。结果,通过整合本研究中使用的不同方法,确定了两个新的潜在地热区域。 (C)2015 Elsevier Ltd.保留所有权利。

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