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首页> 外文期刊>Journal of Volcanology and Geothermal Research >Underwater and drone based photogrammetry reveals structural control at Geysir geothermal field in Iceland
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Underwater and drone based photogrammetry reveals structural control at Geysir geothermal field in Iceland

机译:基于水下和无人机的摄影测量揭示了冰岛盖西尔地热田的结构控制

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摘要

Geysers are local hydrothermal vents with periodic gas bubble driven explosions at the surface. little is known, however, on the control on distribution, the dynamics and the geometry of the conduits of geysers. To better understand the link between the deep and surface expression at the Geysir geothermal field, Iceland, a detailed analysis of the spatial distribution of the thermal expressions, and their relationship to the tectonic framework was carried out. By use of high resolution unmanned aerial vehicle (UAV) based optical and radiometric infrared cameras, we are able to identify 364 distinct thermal spots distributed over the area. Close analysis of their arrangement yields a clustered appearance, following a preferred direction that is found to be consistent with the assumed tectonic trend in the area. Furthermore by using underwater cameras we are able to obtain for the first time detailed images from the two largest geysers at depths exceeding 20 m. Near to the surface, the conduit of the geysers are near circular, but at a depth of 9-12 m the shape changes into a crack-like elongated fissure. The elongation direction of these deep cracks is consistent with the identified thermal expression at the surface, highlighting a structural or even tectonic control at the Geysir geothermal field, which may also explain the susceptibility for seismically triggered activity changes. (C) 2018 Elsevier B.V. All rights reserved.
机译:间歇泉是局部热液喷口,表面周期性地有气泡驱动的爆炸。然而,关于间歇喷泉的分布,动力学和几何形状的控制知之甚少。为了更好地了解冰岛盖西尔地热场的深层表达与地表表达之间的联系,对热表达的空间分布及其与构造框架的关系进行了详细分析。通过使用基于高分辨率无人飞行器(UAV)的光学和辐射红外摄像机,我们能够识别364个分布在该区域的不同热点。仔细分析它们的排列,会发现一个聚集的外观,遵循一个优选的方向,该方向与该地区的假定构造趋势相一致。此外,通过使用水下摄像机,我们能够首次从两个最大的间歇泉获得深度超过20 m的详细图像。间歇泉的导管接近地面,呈圆形,但在9-12 m的深度,其形状变成了裂纹状的细长裂缝。这些深裂缝的延伸方向与确定的地表热表达相一致,突显了盖西尔地热田的结构控制甚至构造控制,这也可能解释了地震触发的活动变化的敏感性。 (C)2018 Elsevier B.V.保留所有权利。

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