Abstract
The Milas Fault (MF) is a poorly understood active fault located between the Büyük Menderes graben to the north and the Gökova graben to the south within the Anatolian–Aegean Region, SW Türkiye. This dextral strike-slip fault has a length of 55 km between Bafa Lake in the northwest and Çamlıca village in the southeast, with a general strike of N60°W, and its surface trace displays two separate geometric segments.
| Original language | English |
|---|---|
| Pages (from-to) | 1639-1662 |
| Number of pages | 24 |
| Journal | Natural Hazards |
| Volume | 116 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - Mar 2023 |
Bibliographical note
Publisher Copyright:© 2023, The Author(s), under exclusive licence to Springer Nature B.V.
Funding
This work was supported by the Scientific and Technological Research Council of Türkiye-TUBITAK (Grant Number 116Y179).
| Funders | Funder number |
|---|---|
| Türkiye Bilimsel ve Teknolojik Araştırma Kurumu | 116Y179 |
Keywords
- Earthquake
- Palaeoseismology
- SW Anatolia
- The Milas Fault
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