Karlıova triple junction: Difference between revisions
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Dadaist6174 (talk | contribs) Corrected a misleading statement not fleshed out about F standing for "fault;" the triple junction article linked in this one states F stands for "transform fault." Clarified the language of the second paragraph and added information on F. |
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{{short description|Place where the Anatolian plate, the Eurasian plate and the Arabian plate meet}} |
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[[File:Anatolian Plate. |
[[File:Anatolian Plate Vectoral.svg|lang=en|thumb|The Karlıova triple junction at the junction of the East and North Anatolian Faults|320px]] |
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The '''Karlıova |
The '''Karlıova triple junction''' is a geologic [[triple junction]] of three [[tectonic]] plates: the [[Anatolian plate]], the [[Eurasian plate]] and the [[Arabian plate]]. |
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==Location== |
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The Karlıova |
The Karlıova triple junction is found where the east–west trending [[North Anatolian Fault]] intersects the [[East Anatolian Fault]] coming up from the southwest, and is ~700 km distant from the [[Maras triple junction]]. Because each arm of the junction is a [[transform fault]] (F), the Karlıova triple junction is an F-F-F type junction.{{clarify|reason=Not clear how a FFF junction is geometrically possible|date=October 2018}} |
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==Geometry== |
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The Karliova triple junction is a geological intersection point located in eastern Turkey, where the boundaries of the Arabian plate, the Eurasian plate, and the African plate meet. It is a complex structure with multiple faults and fractures, resulting from the collision and convergence of these tectonic plates. |
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The geometry of the Karliova triple junction is characterized by three intersecting arms, each representing the boundary of one of the plates. The arms meet at an angle of approximately 120 degrees, forming a Y-shaped configuration. The Arabian plate boundary extends to the southeast, the African plate boundary extends to the southwest, and the Eurasian plate boundary extends to the north.<ref name="Geometry of K.T.J Source 1">{{cite web |last1=Bird |first1=Peter |title=Bird, P. (2003). An updated digital model of plate boundaries. |url=https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2001GC000252 |website=AGU.org |publisher=AGU Publications |access-date=26 October 2023}}</ref><ref name="Geometry of K.T.J Source 2">{{cite web |last1=Karaoğlu |first1=Özgür |last2=Sağlam Selçuk |first2=Azad |last3=Gudmundsson |first3=Agust |title=Tectonic controls on the Karlıova triple junction (Turkey): Implications for tectonic inversion and the initiation of volcanism. |url=https://www.sciencedirect.com/science/article/abs/pii/S0040195116305352 |website=Science Direct |publisher=Science Direct |access-date=26 October 2023}}</ref> |
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==References== |
==References== |
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{{Reflist}} |
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* [http://www.cosis.net/abstracts/EGU2007/06822/EGU2007-J-06822.pdf "New constraints on the Karliova Triple Junction between Arabia, Eurasia and Anatolia", A. Hubert-Ferrari, Geophysical Research Abstracts, Vol. 9, 06822, 2007.] |
* [http://www.cosis.net/abstracts/EGU2007/06822/EGU2007-J-06822.pdf "New constraints on the Karliova Triple Junction between Arabia, Eurasia and Anatolia", A. Hubert-Ferrari, Geophysical Research Abstracts, Vol. 9, 06822, 2007.] |
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* [http://www.koeri.boun.edu.tr/depremmuh/eski/eqspecials/bingol/bingol_eq.htm#TECTONICS%C2%A0OF%20THE%20REGION MAY 1, 2003 BİNGÖL (TURKEY) EARTHQUAKE, Preliminary Report (Updated on May 13, 2003)] |
* [https://web.archive.org/web/20110524000948/http://www.koeri.boun.edu.tr/depremmuh/eski/eqspecials/bingol/bingol_eq.htm#TECTONICS%C2%A0OF%20THE%20REGION MAY 1, 2003 BİNGÖL (TURKEY) EARTHQUAKE, Preliminary Report (Updated on May 13, 2003)] |
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{{Triple Junctions}} |
{{Triple Junctions}} |
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[[Category:Triple junctions]] |
[[Category:Triple junctions]] |
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[[Category:Plate tectonics]] |
[[Category:Plate tectonics]] |
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[[Category: |
[[Category:Geology of Turkey]] |
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Latest revision as of 21:53, 11 November 2024
The Karlıova triple junction is a geologic triple junction of three tectonic plates: the Anatolian plate, the Eurasian plate and the Arabian plate.
Location
[edit]The Karlıova triple junction is found where the east–west trending North Anatolian Fault intersects the East Anatolian Fault coming up from the southwest, and is ~700 km distant from the Maras triple junction. Because each arm of the junction is a transform fault (F), the Karlıova triple junction is an F-F-F type junction.[clarification needed]
Geometry
[edit]The Karliova triple junction is a geological intersection point located in eastern Turkey, where the boundaries of the Arabian plate, the Eurasian plate, and the African plate meet. It is a complex structure with multiple faults and fractures, resulting from the collision and convergence of these tectonic plates.
The geometry of the Karliova triple junction is characterized by three intersecting arms, each representing the boundary of one of the plates. The arms meet at an angle of approximately 120 degrees, forming a Y-shaped configuration. The Arabian plate boundary extends to the southeast, the African plate boundary extends to the southwest, and the Eurasian plate boundary extends to the north.[1][2]
References
[edit]- ^ Bird, Peter. "Bird, P. (2003). An updated digital model of plate boundaries". AGU.org. AGU Publications. Retrieved 26 October 2023.
- ^ Karaoğlu, Özgür; Sağlam Selçuk, Azad; Gudmundsson, Agust. "Tectonic controls on the Karlıova triple junction (Turkey): Implications for tectonic inversion and the initiation of volcanism". Science Direct. Science Direct. Retrieved 26 October 2023.
- "New constraints on the Karliova Triple Junction between Arabia, Eurasia and Anatolia", A. Hubert-Ferrari, Geophysical Research Abstracts, Vol. 9, 06822, 2007.
- MAY 1, 2003 BİNGÖL (TURKEY) EARTHQUAKE, Preliminary Report (Updated on May 13, 2003)
| Triple trench | |
|---|---|
| Triple ridge | |
| Triple fault | |
| Trench–trench–ridge | |
| Fault–fault–trench | |
| Ridge–fault–fault | |
| Ridge–trench–fault | |
| See also | |
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