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Journal articles on the topic 'Anatolian Plateau'

Author: Grafiati

Published: 4 June 2021

Last updated: 3 February 2022

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1

Özdoğan, Mehmet. "Amidst Mesopotamia-centric and Euro-centric approaches: the changing role of the Anatolian peninsula between the East and the West." Anatolian Studies 57 (December 2007): 17–24. http://dx.doi.org/10.1017/s0066154600008462.

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AbstractDue to its geographical position, the Anatolian plateau has always been considered as a bridge in transmitting cultural formations that originated in the Near East to southeastern Europe and to the Aegean. Such a standpoint downgrades the role played by the Anatolian plateau to a transit route between the East and the West, overlooking its distinct structure. It seems that the main bias is in considering the Anatolian plateau as a single cultural unit, ignoring the multifarious nature of its structure. The role the Anatolian plateau played between the ‘East’ and the ‘West’ was much mor

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Steadman, Sharon R., Gregory McMahon, Benjamin S. Arbuckle, et al. "Stability and change at Çadır Höyük in central Anatolia: a case of Late Chalcolithic globalisation?" Anatolian Studies 69 (2019): 21–57. http://dx.doi.org/10.1017/s0066154619000036.

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AbstractScholars have recently investigated the efficacy of applying globalisation models to ancient cultures such as the fourth-millennium BC Mesopotamian Uruk system. Embedded within globalisation models is the ‘complex connectivity‘ that brings disparate regions together into a singular world. In the fourth millennium BC, the site of Çadır Höyük on the north-central Anatolian plateau experienced dramatic changes in its material culture and architectural assemblages, which in turn reflect new socio-economic, sociopolitical and ritual patterns at this rural agro-pastoral settlement. This stud

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Bikoulis, Peter. "Revisiting prehistoric sites in the Göksu valley: a GIS and social network approach." Anatolian Studies 62 (November 13, 2012): 35–59. http://dx.doi.org/10.1017/s0066154612000026.

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AbstractUsing a variety of quantitative approaches, interactions between prehistoric sites in the Göksu valley and south-central Anatolia are modelled within their wider multi-regional and diachronic socio-economic networks to assess the prominence and influence of communities in south-central Anatolia from the Late Chalcolithic to the end of the Early Bronze Age (c. 4200–2000 BC). Since the 1950s, some have understood the valley as significant in terms of movement and communication through the Taurus mountain chain that divides the southern Anatolian plateau from the Mediterranean coast. This

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Summers, Geoffrey D. "The Median Empire reconsidered: a view from Kerkenes Dağ." Anatolian Studies 50 (December 2000): 55–74. http://dx.doi.org/10.2307/3643014.

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SummaryThe city on the Kerkenes Dağ in central Anatolia is the largest pre-Hellenistic urban centre on the plateau (figs 1–2). It has plausibly been identified with a city of the Medes, called Pteria by Herodotus (1.76). If the identification is accepted, the city represents an expansion and imposition of Iranian power over the northern part of the central plateau. Kerkenes might thus provide evidence concerning the first sustained cultural, political and military contact between an Iranian imperial regime and Anatolian powers. Unique circumstances and developing technologies are providing an

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Brocard, Gilles Y., Maud J. M. Meijers, Michael A. Cosca, et al. "Fast Pliocene integration of the Central Anatolian Plateau drainage: Evidence, processes, and driving forces." Geosphere 17, no. 3 (2021): 739–65. http://dx.doi.org/10.1130/ges02247.1.

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Abstract Continental sedimentation was widespread across the Central Anatolian Plateau in Miocene–Pliocene time, during the early stages of plateau uplift. Today, however, most sediment produced on the plateau is dispersed by a well-integrated drainage and released into surrounding marine depocenters. Residual long-term (106–107 yr) sediment storage on the plateau is now restricted to a few closed catchments. Lacustrine sedimentation was widespread in the Miocene–Pliocene depocenters. Today, it is also restricted to the residual closed catchments. The present-day association of closed catchmen

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Erpehlivan, Hüseyin. "Anatolian-Persian grave stelae from Bozüyük in Phrygia: a contribution to understanding Persian presence and organisation in the region." Anatolian Studies 71 (2021): 59–74. http://dx.doi.org/10.1017/s0066154621000053.

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AbstractThis paper provides an assessment of four grave stelae that were found recently in the area surrounding Bozüyük, on the Anatolian plateau in the south of the Bilecik province. The plateau was part of the core of the kingdom of Phrygia during the Early and Middle Iron Ages, and part of the satrapy of Phrygia during the Achaemenid period of the Late Iron Age in Anatolia. The main focus is to examine the place of such stelae among Anatolian-Persian examples and to explore elements of Persian presence and organisation in the region. The precise archaeological contexts of these stelae are u

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Baird, Douglas, Andrew Fairbairn, Emma Jenkins, et al. "Agricultural origins on the Anatolian plateau." Proceedings of the National Academy of Sciences 115, no. 14 (2018): E3077—E3086. http://dx.doi.org/10.1073/pnas.1800163115.

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This paper explores the explanations for, and consequences of, the early appearance of food production outside the Fertile Crescent of Southwest Asia, where it originated in the 10th/9th millennia cal BC. We present evidence that cultivation appeared in Central Anatolia through adoption by indigenous foragers in the mid ninth millennium cal BC, but also demonstrate that uptake was not uniform, and that some communities chose to actively disregard cultivation. Adoption of cultivation was accompanied by experimentation with sheep/goat herding in a system of low-level food production that was int

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ŞIRIN, DENIZ, MEHMET SAIT TAYLAN, RIFAT BIRCAN, GÜRKAN AKYILDIZ, and LEVENT CAN. "Phylogenetic and phylogeographic analysis of Myrmeleotettix maculatus (Orthoptera: Acrididae: Gomphocerinae) species group in Anatolia." Zootaxa 4949, no. 1 (2021): 149–62. http://dx.doi.org/10.11646/zootaxa.4949.1.8.

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Six Anatolian and one European populations of the Myrmeleotettix maculatus species group, which contains M. maculatus and M. ethicus species, have been studied by using molecular genetics methods with mitochondrial COI gene. Myrmeleotettix ethicus is an Anatolian endemic species with local distribution whereas M. maculatus is distributed in western Palearctic. The phylogenetic analysis (ML and BI analyses) of the M. maculatus species group in Anatolia reveals that it consistently recovered two well-supported main clades and four different lineages. Molecular time estimates suggest that the div

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Massa, Michele, Orlene McIlfatrick, and Erkan Fidan. "Patterns of metal procurement, manufacture and exchange in Early Bronze Age northwestern Anatolia: Demircihüyük and beyond." Anatolian Studies 67 (2017): 51–83. http://dx.doi.org/10.1017/s0066154617000084.

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AbstractThis paper adds a new interpretive layer to the already extremely well-investigated site of Demircihüyük, a small Early Bronze Age settlement at the northwestern fringes of the central Anatolian plateau. It presents a reassessment of the evidence for prehistoric mining in the region, as well as a new programme of chemical composition analysis integrated with an object functional and technological typology of the site's metal assemblages. The results reveal complex manufacturing techniques (such as bivalve mould casting, plating and lost wax) and the co-occurrence of several alloying ty

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Özsayin, Erman, and Kadir Dirik. "The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extension." Geologica Carpathica 62, no. 4 (2011): 345–59. http://dx.doi.org/10.2478/v10096-011-0026-7.

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The role of oroclinal bending in the structural evolution of the Central Anatolian Plateau: evidence of a regional changeover from shortening to extensionThe NW-SE striking extensional Inönü-Eskişehir Fault System is one of the most important active shear zones in Central Anatolia. This shear zone is comprised of semi-independent fault segments that constitute an integral array of crustal-scale faults that transverse the interior of the Anatolian plateau region. The WNW striking Eskişehir Fault Zone constitutes the western to central part of the system. Toward the southeast, this system splays

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11

Bottema, Sytze. "Late Quaternary and modern distribution of forest and some tree taxa in Turkey." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 89 (1986): 103–11. http://dx.doi.org/10.1017/s0269727000008940.

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SynopsisA broad outline is presented of forest distribution in Turkey during the last 15,000 years, based upon palynological evidence. The history of some selected taxa is given in more detail and compared with present day distributions. Considerable differences in forest composition were found between the mountain ranges N of the Anatolian plateau, the ranges S and SW of the plateau and the area SE of the eastern (Cilician) Taurus. Pinus dominated the northern part during most of the Late Glacial and the Holocene. In southwestern Anatolia a strong increase of Pinus halted SE of the Konya plai

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12

Spataro, M., A. Fletcher, C. R. Cartwright, and D. Baird. "Boncuklu Höyük: The earliest ceramics on the Anatolian plateau." Journal of Archaeological Science: Reports 16 (December 2017): 420–29. http://dx.doi.org/10.1016/j.jasrep.2016.10.011.

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13

Meijers, Maud J. M., Gilles Y. Brocard, Donna L. Whitney, and Andreas Mulch. "Paleoenvironmental conditions and drainage evolution of the central Anatolian lake system (Turkey) during late Miocene to Pliocene surface uplift." Geosphere 16, no. 2 (2020): 490–509. http://dx.doi.org/10.1130/ges02135.1.

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Abstract Continued Africa-Eurasia convergence resulted in post–11 Ma surface uplift of the Central Anatolian Plateau (CAP) and the westward escape of the Anatolian microplate. Contemporaneously, a central Anatolian fluvio-lacustrine system developed that covered extensive parts of the rising CAP. Today, the semi-arid CAP interior—except for the Konya closed catchment—drains toward the Black Sea, the Mediterranean Sea, and the Persian Gulf. Lake connectivity and drainage patterns of the fluvio-lacustrine system in the evolving plateau region are, however, largely unknown. Here, we present sedim

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Topuz, Gültekin, Osman Candan, Thomas Zack, and Ali Yılmaz. "East Anatolian plateau constructed over a continental basement: No evidence for the East Anatolian accretionary complex." Geology 45, no. 9 (2017): 791–94. http://dx.doi.org/10.1130/g39111.1.

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15

Barbot, S., and J. R. Weiss. "Connecting subduction, extension and shear localization across the Aegean Sea and Anatolia." Geophysical Journal International 226, no. 1 (2021): 422–45. http://dx.doi.org/10.1093/gji/ggab078.

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SUMMARY The Eastern Mediterranean is the most seismically active region in Europe due to the complex interactions of the Arabian, African, and Eurasian tectonic plates. Deformation is achieved by faulting in the brittle crust, distributed flow in the viscoelastic lower-crust and mantle, and Hellenic subduction, but the long-term partitioning of these mechanisms is still unknown. We exploit an extensive suite of geodetic observations to build a kinematic model connecting strike-slip deformation, extension, subduction, and shear localization across Anatolia and the Aegean Sea by mapping the dist

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Atalar, Müge, Marianna Kováčová, Mine Sezgül Kayseri Özer, and Torsten Utescher. "Late Messinian palynoflora from Central Anatolian Plateau (Çankırı Basin) [abstract]." Geology, Geophysics & Environment 42, no. 1 (2016): 57. http://dx.doi.org/10.7494/geol.2016.42.1.57.

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17

Yakar, Jak. "Regional and Local Schools of Metalwork in Early Bronze Age Anatolia Part II." Anatolian Studies 35 (December 1985): 25–38. http://dx.doi.org/10.2307/3642869.

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This is one of the most eventful periods in the early history of preliterate Anatolia. Urban and rural settlements in western Anatolia, in the central Anatolian plateau including the Pontus region and in the eastern highlands show signs of conflagration. Archaeological surveys carried out in north-central Anatolia and in the Konya plain suggest that in some cases permanent settlements were abandoned at different phases of the EB III. These destructions were no doubt caused by unrecorded events such as inter-regional rivalry between city-states, intruding pastoralists, incursions by foreign arm

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18

Luke, Christina, and Elvan Cobb. "Dwelling in Hacıveliler: social-engineering policies in the context of space, place and landscape in rural, western Turkey." Anatolian Studies 63 (July 11, 2013): 155–73. http://dx.doi.org/10.1017/s0066154613000082.

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AbstractThe Gediz valley of modern, western Turkey is a major gateway linking the Aegean spheres with the central Anatolian plateau. The making of cultural heritage in Anatolia plays out in very different ways depending on the physical location of the community and the level of implementation of the post-1923 social- and political-engineering agendas of the authorities of the Republic of Turkey. In this case-study we analyse one community, a village of just under 200 people known as Hacıveliler in the Marmara Lake basin of the Gediz valley in western Turkey (province of Manisa). We explore how

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Chronis, Themis, Dionysios E. Raitsos, Dimitris Kassis, and Athanassios Sarantopoulos. "The Summer North Atlantic Oscillation Influence on the Eastern Mediterranean." Journal of Climate 24, no. 21 (2011): 5584–96. http://dx.doi.org/10.1175/2011jcli3839.1.

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Abstract This study highlights an important and previously overlooked summer North Atlantic Oscillation (NAO) influence over the eastern Mediterranean. The featured analysis is based on a synergistic use of reanalysis data, satellite retrievals, and coastal and buoy meteorological observations. The physical mechanisms at play reveal a strong summer NAO involvement on the pressure fields over northern Europe and the Anatolian plateau. Especially during August, the summer NAO modulates the Anatolian low, together with the air temperature, meridional atmospheric circulation, and cloudiness over t

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Krystopowicz, Neil J., Lindsay M. Schoenbohm, Jeremy Rimando, Gilles Brocard, and Bora Rojay. "Tectonic geomorphology and Plio-Quaternary structural evolution of the Tuzgölü fault zone, Turkey: Implications for deformation in the interior of the Central Anatolian Plateau." Geosphere 16, no. 5 (2020): 1107–24. http://dx.doi.org/10.1130/ges02175.1.

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Abstract Situated within the interior of the Central Anatolian Plateau (Turkey), the 200-km-long Tuzgölü extensional fault zone offers first-order constraints on the timing and pattern of regional deformation and uplift. In this study, we analyze the morphometrics of catchments along the Tuzgölü range-front fault and the parallel, basinward Hamzalı fault using a variety of measured morphometric indicators coupled with regional geomorphic observations and longitudinal profile analysis. In addition, we use field and remote mapping to constrain the geometry of two key marker beds, the Pliocene Kı

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21

Ahmadzadeh, Faraham, Aziz Avcı, Farhang Torki, Çetin Ilgaz, and Yusuf Kumlutaş. "Description of four new Asaccus Dixon and Anderson, 1973 (Reptilia: Phyllodactylidae) from Iran and Turkey." Amphibia-Reptilia 32, no. 2 (2011): 185–202. http://dx.doi.org/10.1163/017353711x556998.

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AbstractOne new Asaccus from the Anatolian plateau and three new Asaccus from the Iranian plateau are described as follows. (1) Asaccus barani sp. nov.: diagnosed by strongly heterogeneous dorsal tubercles; (2) Asaccus iranicus sp. nov.: diagnosed by small body size and digits (forelimbs) parallel joint to palm; (3) Asaccus tangestanensis sp. nov.: by having enlarged trihedral tubercles all over the dorsal body; (4) Asaccus zagrosicus sp. nov.: secondary postmentals are not in contact with lowerlabials (100% of specimens). Other important data on the new Asaccus are given in detail in the text

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Hopkins, David C. "Across the Anatolian Plateau: Readings in the Archaeology of Ancient Turkey." Annual of the American Schools of Oriental Research 57 (2000): i. http://dx.doi.org/10.2307/3768580.

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AYDAR, Erkan, H. Evren ÇUBUKÇU, Erdal ŞEN, and Lütfiye AKIN. "Central Anatolian Plateau, Turkey: incision and paleoaltimetry recorded from volcanic rocks." TURKISH JOURNAL OF EARTH SCIENCES 22 (2013): 739–46. http://dx.doi.org/10.3906/yer-1211-8.

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Sahin, Sakir, Xueyang Bao, Niyazi Turkelli, Eric Sandvol, Ugur Teoman, and Metin Kahraman. "Lg Wave Attenuation in the Isparta Angle and Anatolian Plateau (Turkey)." Pure and Applied Geophysics 170, no. 3 (2012): 337–51. http://dx.doi.org/10.1007/s00024-012-0517-1.

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Meijers, Maud J. M., Gilles Y. Brocard, Michael A. Cosca, et al. "Rapid late Miocene surface uplift of the Central Anatolian Plateau margin." Earth and Planetary Science Letters 497 (September 2018): 29–41. http://dx.doi.org/10.1016/j.epsl.2018.05.040.

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Steadman, Sharon R., Benjamin S. Arbuckle, and Gregory McMahon. "Pivoting East." Documenta Praehistorica 45 (January 3, 2019): 64–85. http://dx.doi.org/10.4312/dp.45-6.

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The investigation of ‘complex connectivities’ as defined by Tomlinson (1999) as a critical element in the understanding of how modern globalization works has been repurposed by archaeologists as a model to explain the mechanisms at work in the archaeological past. This study applies Tomlinson’s model to interpret evidence that such connectivities linked the vast Uruk system in Mesopotamia, the contemporary Kura-Araxes culture in Transcaucasia, and the north central Anatolian plateau in the second half of the fourth millennium BCE, known as the Late Chalcolithic period. We focus on the site of

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Steadman, Sharon R., Benjamin S. Arbuckle, and Gregory McMahon. "Pivoting East." Documenta Praehistorica 45 (December 29, 2018): 64–85. http://dx.doi.org/10.4312/dp.45.6.

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The investigation of ‘complex connectivities’ as defined by Tomlinson (1999) as a critical element in the understanding of how modern globalization works has been repurposed by archaeologists as a model to explain the mechanisms at work in the archaeological past. This study applies Tomlinson’s model to interpret evidence that such connectivities linked the vast Uruk system in Mesopotamia, the contemporary Kura-Araxes culture in Transcaucasia, and the north central Anatolian plateau in the second half of the fourth millennium BCE, known as the Late Chalcolithic period. We focus on the site of

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Najibzadeh, Masoumeh, Michael Veith, Ahmad Gharzi, et al. "Molecular phylogenetic relationships among Anatolian-Hyrcanian brown frog taxa (Ranidae: Rana)." Amphibia-Reptilia 38, no. 3 (2017): 339–50. http://dx.doi.org/10.1163/15685381-00003114.

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Although the phylogenetic relationship of Western Palearctic brown frogs has been repeatedly studied, the taxonomic status and phylogenetic relationship of Anatolian-Hyrcanian brown frogs is still not fully resolved. Here, we assess the phylogenetic status of these species among Western Palearctic brown frogs with special emphasize on Iranian populations based on two partial mitochondrial DNA sequences (16S rRNA and cytochrome b genes) and the application of a molecular clock. Our results clearly show that Western Palearctic brown frogs underwent a basal radiation in to two main monophyletic c

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Reid, M. R., J. R. Delph, M. A. Cosca, W. K. Schleiffarth, and G. Gençalioğlu Kuşcu. "Melt equilibration depths as sensors of lithospheric thickness during Eurasia-Arabia collision and the uplift of the Anatolian Plateau." Geology 47, no. 10 (2019): 943–47. http://dx.doi.org/10.1130/g46420.1.

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Abstract A co-investigation of mantle melting conditions and seismic structure revealed an evolutionary record of mantle dynamics accompanying the transition from subduction to collision along the Africa-Eurasia margin and the >1 km uplift of the Anatolian Plateau. New 40Ar/39Ar dates of volcanic rocks from the Eastern Taurides (southeast Turkey) considerably expand the known spatial extent of Miocene-aged mafic volcanism following a magmatic lull over much of Anatolia that ended at ca. 20 Ma. Mantle equilibration depths for these chemically diverse basalts are interpreted to indicate that

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Yilmaz, Ali, Hüseyin Yilmaz, Cemal Kaya, and Durmus Boztug. "The Nature of the Crustal Structure of the Eastern Anatolian Plateau, Turkey." Geodinamica Acta 23, no. 4 (2010): 167–83. http://dx.doi.org/10.3166/ga.23.167-183.

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Bartol, J., and R. Govers. "A single cause for uplift of the Central and Eastern Anatolian plateau?" Tectonophysics 637 (December 2014): 116–36. http://dx.doi.org/10.1016/j.tecto.2014.10.002.

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Balliance, D. K. "SUMMER OBSERVATIONS ON THE BIRDS OF THE ANATOLIAN PLATEAU AND NORTHWESTERN CILICIA." Ibis 100, no. 4 (2008): 617–20. http://dx.doi.org/10.1111/j.1474-919x.1958.tb07964.x.

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Ozacar, A. Arda, Hersh Gilbert, and George Zandt. "Upper mantle discontinuity structure beneath East Anatolian Plateau (Turkey) from receiver functions." Earth and Planetary Science Letters 269, no. 3-4 (2008): 427–35. http://dx.doi.org/10.1016/j.epsl.2008.02.036.

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Gökalp, Hüseyin. "Tomographic Imaging of the Seismic Structure Beneath the East Anatolian Plateau, Eastern Turkey." Pure and Applied Geophysics 169, no. 10 (2011): 1749–76. http://dx.doi.org/10.1007/s00024-011-0432-x.

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McPhee, Peter J., Douwe J. J. van Hinsbergen, and Stuart N. Thomson. "Thermal history of the western Central Taurides fold-thrust belt: Implications for Cenozoic vertical motions of southern Central Anatolia." Geosphere 15, no. 6 (2019): 1927–42. http://dx.doi.org/10.1130/ges02164.1.

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Abstract The modern physiography of central Turkey is dominated by the 1-km-high Central Anatolian Plateau and the Central Tauride mountains that form the southern plateau margin. These correspond to a Cretaceous–Eocene backarc extensional province and forearc fold-thrust belt, respectively. The extent to which the morphology of the Miocene plateau was inherited from the physiography of the Cretaceous–Eocene subduction zone that assembled the Anatolian crust has not been tested but is important if we are to isolate the signal of Miocene and younger subduction dynamics in the formation of the m

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Massa, Michele. "Early Bronze Age burial customs on the central Anatolian plateau: a view from Demircihöyük-Sarıket." Anatolian Studies 64 (2014): 73–93. http://dx.doi.org/10.1017/s0066154614000064.

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AbstractThis paper focuses on the analysis of the cemetery of Demircihöyük-Sarıket, for which exists one of the largest Early Bronze Age funerary datasets published to date in Anatolia. The size and quality of the sample allow the dataset to be approached quantitatively, to determine both normative and anomalous funerary practices, and to detect distinct patterns of burial treatment for different segments of the population represented in the cemetery. Despite the small size of the community (ca 100–130 people), the results suggest a rather complex picture, in which the choice of specific buria

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RAMSAY, L. N. G. "Observations on the Bird-Life of the Anatolian Plateau during the Summer of 1907." Ibis 56, no. 3 (2008): 365–87. http://dx.doi.org/10.1111/j.1474-919x.1914.tb04076.x.

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Schemmel, F., T. Mikes, B. Rojay, and A. Mulch. "The impact of topography on isotopes in precipitation across the Central Anatolian Plateau (Turkey)." American Journal of Science 313, no. 2 (2013): 61–80. http://dx.doi.org/10.2475/02.2013.01.

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Yildirim, Cengiz, Daniel Melnick, Paolo Ballato, et al. "Differential uplift along the northern margin of the Central Anatolian Plateau: inferences from marine terraces." Quaternary Science Reviews 81 (December 2013): 12–28. http://dx.doi.org/10.1016/j.quascirev.2013.09.011.

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Makkouk, K. M., L. Bertschinger, M. Conti, N. Bolay, and F. Dusunceli. "Barley Yellow Striate Mosaic Rhabdovirus Naturally Infects Cereal Crops in the Anatolian Plateau of Turkey." Journal of Phytopathology 144, no. 7-8 (1996): 413–15. http://dx.doi.org/10.1111/j.1439-0434.1996.tb00315.x.

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Özacar, A. Arda, George Zandt, Hersh Gilbert, and Susan L. Beck. "Seismic images of crustal variations beneath the East Anatolian Plateau (Turkey) from teleseismic receiver functions." Geological Society, London, Special Publications 340, no. 1 (2010): 485–96. http://dx.doi.org/10.1144/sp340.21.

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Steadman, Sharon R., Jennifer C. Ross, Gregory McMahon, and Ronald L. Gorny. "Excavations on the north-central plateau: The Chalcolithic and Early Bronze Age occupation at Çadır Höyük." Anatolian Studies 58 (December 2008): 47–86. http://dx.doi.org/10.1017/s0066154600008668.

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AbstractThe last decade of excavations at Çadır Höyük, in the north-central region of the Anatolian plateau, has revealed a well-established Late Chalcolithic community with continuous occupation into the Early Bronze I period (mid fourth to early third millennium BC). While the Late Chalcolithic town was prosperous, with well-made houses and objects, and even monumental construction, the stability of the settlement had slipped by the Early Bronze I phase. We summarise here the results from ten seasons of work at the site and profile how the findings contribute to our understanding of Çadır's

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Karabulut, Hayrullah, Anne Paul, Ali Değer Özbakır, Tuğçe Ergün, and Selver Şentürk. "A new crustal model of the Anatolia–Aegean domain: evidence for the dominant role of isostasy in the support of the Anatolian plateau." Geophysical Journal International 218, no. 1 (2019): 57–73. http://dx.doi.org/10.1093/gji/ggz147.

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Steadman, Sharon R. "Heading Home: The Architecture of Family and Society in Early Sedentary Communities on the Anatolian Plateau." Journal of Anthropological Research 60, no. 4 (2004): 515–58. http://dx.doi.org/10.1086/jar.60.4.3631140.

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Oruç, Bülent, Oya Pamukçu, and Tuba Sayın. "Isostatic Moho undulations and estimated elastic thicknesses of the lithosphere in the central Anatolian plateau, Turkey." Journal of Asian Earth Sciences 170 (February 2019): 166–73. http://dx.doi.org/10.1016/j.jseaes.2018.11.001.

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Cosentino, D., T. F. Schildgen, P. Cipollari, et al. "Late Miocene surface uplift of the southern margin of the Central Anatolian Plateau, Central Taurides, Turkey." Geological Society of America Bulletin 124, no. 1-2 (2011): 133–45. http://dx.doi.org/10.1130/b30466.1.

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Crespin, Anne-Sophie. "Between Phrygia and Cilicia: the Porsuk area at the beginning of the Iron Age." Anatolian Studies 49 (December 1999): 61–72. http://dx.doi.org/10.2307/3643062.

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Abstract:

Porsuk is strategically situated in the northern foothills of the Taurus mountains (see map, fig 1), controlling one of the most important passes between Cilicia and the Anatolian plateau. It seems that this area, which was in the sphere of Hittite culture during the Late Bronze Age, turns towards the southern regions of Cilicia during Porsuk period IV. We shall firstly re-examine the evidence for the Early Iron Age at Porsuk in the light of recent discoveries from a number of other sites. We will then examine evidence that might demonstrate relations between Porsuk IV and Cilicia.During subse

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Yildirim, Cengiz, Taylor F. Schildgen, Helmut Echtler, Daniel Melnick, and Manfred R. Strecker. "Late Neogene and active orogenic uplift in the Central Pontides associated with the North Anatolian Fault: Implications for the northern margin of the Central Anatolian Plateau, Turkey." Tectonics 30, no. 5 (2011): n/a. http://dx.doi.org/10.1029/2010tc002756.

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Öğretmen, Nazik, Virgilio Frezza, Natália Hudáčková, et al. "Early Pleistocene (Calabrian) marine bottom oxygenation and palaeoclimate at the southern margin of the Central Anatolian Plateau." Italian Journal of Geosciences 137, no. 3 (2018): 425–64. http://dx.doi.org/10.3301/ijg.2018.19.

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Görüm, Tolga. "Tectonic, topographic and rock-type influences on large landslides at the northern margin of the Anatolian Plateau." Landslides 16, no. 2 (2018): 333–46. http://dx.doi.org/10.1007/s10346-018-1097-7.

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