Determination of the deep fault geometry along the southern branch of the North Anatolian Fault System by using resistivity and magnetic methods
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- 作者：Metin Aşcıa ; masci@kocaeli.edu.tr" class="auth_mail" title="E-mail the corresponding author ; metin_asci@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; Bü ; lent Doğanb ; Tü ; rker Yasc ; Deniz Ç ; akaa
- 关键词：Wenner lateral resistivity method ; Magnetic dyke method ; Southern branch of the North Anatolian Fault System ; Transtensional stress ; Neotectonic period
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 August 2016
- 年：2016
- 卷：125
- 期：Complete
- 页码：117-137
- 全文大小：13783 K
文摘
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Foothills of highlands are defined by right lateral strike-slip fault.
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The dipping angles of the faults on the surface are similar to those located in the shallower and deep parts of the continental crust.
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The faults in the deep parts of crust are the transtensional stresses components of the strike-slip faulting.
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Comparison of the positioning of the faults in the deep parts of the continental crust to those observed on the surface indicate a fault zone related to strike-slip tectonic system in the region.