Palaeomagnetic study of the Galatean Volcanic Province, north-central Turkey: neogene deformation at the northern border of the Anatolian Block

1999 ◽  
Vol 34 (1-2) ◽  
pp. 7-23 ◽  
Author(s):  
Hal??l Gürsoy ◽  
John D. A. Piper ◽  
Orhan Tatar
Keyword(s):  
North Central ◽  
Volcanic Province ◽  
Northern Border ◽  
Central Turkey

Growth rates of early Campanianrudists in a siliciclastic-calcareous setting (Pontid MTS., North-Central Turkey)

Geobios ◽  
1998 ◽  
Vol 31 ◽  
pp. 385-401 ◽  
Author(s):  
Thomas Steuber ◽  
Cemil Yilmaz ◽  
Hannes Löser
Keyword(s):  
Growth Rates ◽  
North Central ◽  
Central Turkey

Fluids along the North Anatolian Fault, Niksar basin, north central Turkey: Insight from stable isotopic and geochemical analysis of calcite veins

2017 ◽  
Vol 101 ◽  
pp. 58-79 ◽  
Author(s):  
Colin P. Sturrock ◽  
Elizabeth J. Catlos ◽  
Nathan R. Miller ◽  
Aykut Akgun ◽  
András Fall ◽  
...  
Keyword(s):  
North Anatolian Fault ◽  
Geochemical Analysis ◽  
North Central ◽  
The North ◽  
Calcite Veins ◽  
Stable Isotopic ◽  
Central Turkey

scholarly journals The First Glyptostroboxylon and Taxodioxylon Descriptions from the Late Miocene of Turkey and Palaeoclimatological Evaluation

2019 ◽  
Vol 75 (2) ◽  
pp. 268-280 ◽  
Author(s):  
Ünal Akkemik ◽  
Nevriye Neslihan Acarca Bayam
Keyword(s):  
Late Miocene ◽  
Early Miocene ◽  
Central Anatolia ◽  
Forest Composition ◽  
Fossil Species ◽  
Volcanic Province ◽  
History Of ◽  
Warm Temperate Forest ◽  
Central Turkey ◽  
Warm Temperate

Taxodioxylon Hartig, (emended by Gothan 1905) was widely described from the late Oligocene of the European part of Turkey (Thrace) and the early Miocene of greater Turkey, Anatolia.,C,. was also described from the early Miocene of central Anatolia. The purpose of this paper is to present a more detailed extended history of these two genera up to the late Miocene (Tortonian) with new descriptions from the Galatean Volcanic Province in central Turkey. The wood identification showed the presence of two fossil species;,D,et B,and,(G,.) G,. In conclusion, the swamp and lowland warm-temperate forest composition including,and,in the Galatean Volcanic Province, continued from the early Miocene (Burdigalian) to the late Miocene (Tortonian).

An arena for cultural contact: Paphlagonia (north-central Turkey) through prehistory

2007 ◽  
Vol 57 ◽  
pp. 25-34 ◽  
Author(s):  
Roger Matthews
Keyword(s):  
Bronze Age ◽  
Raw Materials ◽  
Early Bronze Age ◽  
Upper Palaeolithic ◽  
Apparent Absence ◽  
North Central ◽  
Cultural Contact ◽  
Long Time ◽  
Time Periods ◽  
Central Turkey

AbstractThe results from five seasons of extensive and intensive survey in north-central Turkey, Project Paphlagonia, are here considered in relation to the prehistory of the region and the broader geographical scene. While the evidence remains limited and patchy it is possible to discern some clear patterns through these long time-periods, which in some respects match those of other regions of Turkey and beyond. They include: a strong Middle Palaeolithic presence; no detectable Upper Palaeolithic or Epi-Palaeolithic sites; an apparent absence of Neolithic settlement; a Chalcolithic settlement pattern that appears to be related to exploitation of raw materials of the region, and; a massive increase in settlement through the centuries of the Early Bronze Age, with evidence for fortification, cemeteries and strong connections to regions well beyond north-central Turkey.

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