scholarly journals Late Pleistocene-Holocene Characteristics of the North Anatolian Fault at Adapazarı Basin. Evidences from the age and geometry of the fluvial terrace staircases

2021 ◽  
Keyword(s):  
Late Pleistocene ◽  
North Anatolian Fault ◽  
Fluvial Terrace ◽  
The North

Quaternary Rock Uplift Rates and Their Implications for the Western Flank of the North Anatolian Fault Restraining Bend; Inferences From Fluvial Terrace Ages

Tectonics ◽  
2020 ◽  
Vol 39 (10) ◽  
Author(s):  
Kevin P. McClain ◽  
Cengiz Yıldırım ◽  
Attila Çiner ◽  
Sefa Şahin ◽  
M. Akif Sarıkaya ◽  
...  
Keyword(s):  
North Anatolian Fault ◽  
Fluvial Terrace ◽  
The North ◽  
Western Flank ◽  
Uplift Rates ◽  
Restraining Bend

scholarly journals The implications of fault zone transformation on aseismic creep: Example of the North Anatolian Fault, Turkey

2017 ◽  
Vol 122 (6) ◽  
pp. 4208-4236 ◽  
Author(s):  
Maor Kaduri ◽  
Jean-Pierre Gratier ◽  
François Renard ◽  
Ziyadin Çakir ◽  
Cécile Lasserre
Keyword(s):  
Fault Zone ◽  
North Anatolian Fault ◽  
The North

A multi-proxy reconstruction of climate during the late-Pleistocene to early Holocene transition in the northeastern, USA

2021 ◽  
pp. 1-17
Author(s):  
Laurie D. Grigg ◽  
Kevin J. Engle ◽  
Alison J. Smith ◽  
Bryan N. Shuman ◽  
Maximilian B. Mandl
Keyword(s):  
Late Pleistocene ◽  
Climatic Variability ◽  
Warming Trend ◽  
Early Holocene ◽  
Individual Species ◽  
Environmental Preferences ◽  
The North ◽  
Show Evidence ◽  
Dry Conditions ◽  
Components Analysis

Abstract A multiproxy record from Twin Ponds, VT, is used to reconstruct climatic variability during the late Pleistocene to early Holocene transition. Pollen, ostracodes, δ18O, and lithologic records from 13.5 to 9.0 cal ka BP are presented. Pollen- and ostracode-inferred climatic reconstructions are based on individual species’ environmental preferences and the modern analog technique. Principal components analysis of all proxies highlights the overall warming trend and centennial-scale climatic variability. During the Younger Dryas cooling event (YD), multiple proxies show evidence for cold winter conditions and increasing seasonality after 12.5 cal ka BP. The early Holocene shows an initial phase of rapid warming with a brief cold interval at 11.5 cal ka BP, followed by a more gradual warming; a cool, wet period from 11.2 to 10.8 cal ka BP; and cool, dry conditions from 10.8 to 10.2 cal ka BP. The record ends with steady warming and increasing moisture. Post-YD climatic variability has been observed at other sites in the northeastern United States and points to continued instability in the North Atlantic during the final phases of deglaciation.

scholarly journals Variations in lithospheric anisotropy across the North Anatolian Fault revealed by teleseismic shear wave splitting

2021 ◽  
Author(s):  
David Cornwell ◽  
Sebastian Rost ◽  
David A Thompson ◽  
Gregory A. Houseman ◽  
Lisa A Millar ◽  
...  
Keyword(s):  
Shear Wave ◽  
Shear Wave Splitting ◽  
North Anatolian Fault ◽  
The North ◽  
Wave Splitting
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