Upper crust response to geodynamic processes beneath Isparta Angle, SW Turkey: Revealed by CMT solutions of earthquakes
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- 作者：Semir Ö ; vera ; semir.over@iste.edu.tr" class="auth_mail" title="E-mail the corresponding author ; Sü ; ha Ö ; zdenb ; Zü ; heyr Kamacıc ; Hü ; seyin Yılmazd ; Ulvi Can Ü ; nlü ; genç ; e ; Ali Pınarf
- 关键词：Inversion ; Stress state ; Earthquake ; Extension ; Isparta Angle ; Upwelling asthenosphere ; SW Anatolia
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：26 September 2016
- 年：2016
- 卷：687
- 期：Complete
- 页码：94-104
- 全文大小：2129 K
文摘
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Present day stress tensor is obtained seismic fault plane solution data
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We obtained E-W extensional stress regime in the Isparta Angle
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The high R value indicates near uniaxial stress state implying that this extension is close radial extension
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We suggest a model to explain E-W extensions in the geodynamical context
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The cause of the E-W extension is the combined forces of the GPE and upwelling hot asthenospheric material.