The Sarikavak Tephra, Galatea, north central Turkey: a case study of a Miocene complex plinian eruption deposit

2001-12-01
Schumacher, R
Mues-Schumacher, U
Toprak, V
Show full item record
Creative Commons License
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
163
views
0
downloads
The Sarikavak Tephra from the central Galatean Volcanic Province (Turkey) represents the deposit of a complex multiple phase plinian eruption of Miocene age. The eruptive sequence is subdivided into the Lower-, Middle-, and Upper Sarikavak Tephra (LSKT, MSKT, USKT) which differ in type of deposits, lithology and eruptive mechanisms.
Galatea, Tephra deposits, Plinian eruption deposits, Eruptive succession
https://hdl.handle.net/11511/67023
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
Department of Geological Engineering, Article

Suggestions

A tsunami generated by a possible submarine slide: Evidence for slope failure triggered by the North Anatolian Fault movement
Minoura, K; Imamura, F; Kuran, U; Nakamura, T; Papadopoulos, GA; Sugawara, D; Takahashi, T; Yalçıner, Ahmet Cevdet (2005-11-01)
A tsunamigenic sediment layer has been discovered in fluvio-alluvial sequences on the northern coast of the Marmara Sea, northwestern Turkey. The layer consists of unsorted silty coarse sand including terrestrial molluscs and charcoal fragments. The AMS radiometric ages of the shells have been estimated at around BC 400, AD 300, AD 400, and AD 1000. We propose that a tsunami occurred in the Marmara Sea in the middle of 11th century and invaded the fluvial plains. The older fossils were derived from the unde...
The Tarakli Flysch in the Boyali area (Sakarya Terrane, northern Turkey): Implications for the tectonic history of the IntraPontide suture zone
Catanzariti, Rita; Ellero, Alessandro; Göncüoğlu, Mehmet Cemal; Marroni, Michele; Ottria, Giuseppe; Pandolfi, Luca (2013-11-01)
In the Boyali area, northern Turkey, the tectonic units of the Istanbul-Zonguldak Terrane and the IntraPontide suture zone are thrust over the deposits at the top of the Sakarya Terrane, known as Tarakli Flysch. It consists of Early Maastrichtian-Middle Paleocene turbidite and mass-gravity deposits, whose source mainly corresponds to the Istanbul-Zonguldak Terrane, and, with a lesser extent, to the IntraPontide suture zone. These deposits were sedimented in a foredeep basin developed during the convergence ...
The Unaz Formation: A Key Unit in the Western Black Sea Region, N Turkey
Tuysuz, Okan; Yılmaz, İsmail Ömer; Svabenicka, Lilian; Kirici, Sabri (2012-01-01)
The Pontide magmatic belt in the Western Pontides, which developed in response to the northward subduction of the northern branches of the Tethys Ocean, consists of two different volcanic successions separated by an Upper Santonian pelagic limestone unit, the Unaz Formation. The first period of volcanism and associated sedimentation started during the Middle Turonian and lasted until the Early Santonian under the control of an extensional tectonic regime, which created horst-graben topography along the sout...
The Kapanbogazi formation: A key unit for understanding Late Cretaceous evolution of the Pontides, N Turkey
TÜYSÜZ, OKAN; Melinte-Dobrinescu, Mihaela C.; Yılmaz, İsmail Ömer; Kirici, Sabri; Svabenicka, Lilian; Skupien, Peter (Elsevier BV, 2016-01-01)
The Pontides forming the south-western continental margin of the Black Sea consist of two tectonic units, the Istanbul Zone in the west, and the Sakarya Zone in the central and eastern parts. The Sinop Basin in the Sakarya Zone is filled, from base to top, by Hauterivian to Albian turbidites, Cenomanian-Turonian red pelagic sediments, Turonian-Campanian magmatic-arc and related deposits, and by the uppermost Campanian to middle Eocene post-magmatic units developed on the southern passive margin of the Black...
The Karakaya Complex: A review of data and concepts
Okay, AI; Göncüoğlu, Mehmet Cemal (2004-05-01)
The Karakaya Complex in the Pontides consists of highly deformed and partly metamorphosed clastic and volcanic series of Permian and Triassic age. It is generally subdivided into two parts: The structurally lower part, called the Lower Karakaya Complex, consists of a mafic lava-mafic pyroclastite-shale-limestone succession metamorphosed in the greenschist and blueschist facies during the Late Palaeozoic or Triassic. The structurally upper part is made up of highly deformed Permian and Triassic clastic, volc...
Citation Formats
R. Schumacher, U. Mues-Schumacher, and V. Toprak, “The Sarikavak Tephra, Galatea, north central Turkey: a case study of a Miocene complex plinian eruption deposit,” JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, pp. 231–245, 2001, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/67023.
METU IIS - Integrated Information Service open@metu.edu.tr