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首页> 外文期刊>Geothermal Energy Science >Convective, intrusive geothermal plays: what about tectonics?
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Convective, intrusive geothermal plays: what about tectonics?

机译:对流侵入性地热演替:构造学呢?

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We revised the concept of convective, intrusive geothermal plays, considering that the tectonic setting is not, in our opinion, a discriminant parameter suitable for a classification. We analysed and compared four case studies: (i) Larderello (Italy), (ii) Mt Amiata (Italy), (iii) The Geysers (USA) and (iv) Kizildere (Turkey). The tectonic settings of these geothermal systems are different and a matter of debate, so it is hard to use this parameter, and the results of classification are ambiguous. We suggest a classification based on the age and nature of the heat source and the related hydrothermal circulation. Finally we propose to distinguish the convective geothermal plays as volcanic, young intrusive and amagmatic.
机译:考虑到构造背景不是适合分类的判别参数,我们修改了对流侵入性地热层的概念。我们分析并比较了四个案例研究:(i)拉德雷洛(意大利),(ii)阿米亚塔山(意大利),(iii)间歇泉(美国)和(iv)基兹尔德雷(土耳其)。这些地热系统的构造背景各不相同,尚有争议,因此很难使用该参数,分类结果也不明确。我们建议根据热源的年龄和性质以及相关的热液循环进行分类。最后,我们建议区分对流地热层为火山岩,年轻侵入岩和岩浆岩。

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