土耳其新构造及其地热意义

IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Bulletin of the Mineral Research and Exploration Pub Date : 2022-12-16 DOI:10.19111/bulletinofmre.1219987

N. Görür, Şebnem Önder

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引用次数: 0

摘要

土耳其新近纪至第四纪新构造时期为地热能开发创造了有利条件。这一时期的主要特征是河流湖相沉积和走滑构造，并伴有岩浆活动。在此条件下，在新构造省(包括北安纳托利亚断裂带和东安纳托利亚断裂带)形成了大量的地热区。今天，土耳其的地热资源主要分布在与地堑系有关的西安纳托利亚伸展省。然而，中安纳托利亚新构造省被认为是最有前途的地热目标之一，其特点是广泛存在热干岩系统。本次研究主要是通过对我国新构造演化的重视，揭示Kırşehir地块这些资源的可能潜力。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Neotectonics of Turkey and its geothermal implication

Favourable conditions for geothermal energy were created in Turkey during its neotectonic episode from Neogene to Quaternary. This episode is characterized mainly by fluvio-lacustrine sedimentation and strike-slip tectonics with associated magmatism. Under these conditions, a great number of geothermal areas have formed in the neotectonic provinces in association with major tectonic features, including the North and East Anatolian Fault Zones (NAFZ and EAFZ, respectively). Today, the geothermal resources of Turkey are mainly located in the West Anatolian Extensional Province associated with the graben systems. However, the Central Anatolian Ova Neotectonic Province is considered as one of the most promising geothermal targets which are characterized by the presence of widespread hot dry rock systems. This study mainly aims to throw light on the possible potentiality of these resources at Kırşehir Block by emphasizing the neotectonic evolution of the country.

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来源期刊

Bulletin of the Mineral Research and Exploration GEOSCIENCES, MULTIDISCIPLINARY-

CiteScore

1.20

自引率

20.00%

发文量

审稿时长

10 weeks

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