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Stratigraphy, Sedimentology and Palynology of the Neogene-Pleistocene(?) Rocks Around Akçaşehir- Tire-İzmir (Küçük Menderes Graben, Western Anatolia)
earth siences rocks gneisses
2011/3/22
The basement rocks located in the central part of the southern edge of the Küçük Menderes Graben, around Akçaşehir-Tire are composed of marbles, schists, gneisses and metagabbros of...
Volcanic Rocks From Foça-Karaburun and Ayvalik-Lesvos grabens (Western Anatolia) and Their Petrogenetic-Geodynamic Significance
Turkish Aegean region volcanic rocks extension tectonics Cenozoic geochemistry petrology
2010/10/14
The Foça-Karaburun and Ayvalık-Lesvos grabens (western coast of Anatolia, Turkey) are two important NW-SE-trending extensional areas generated in response to the Early Miocene-Holocene ext...
Mafic Microgranular Enclaves in the Kozak Granodiorite, Western Anatolia
Kozak Granodiorite Western Anatolia
2009/7/8
Enclaves which are relicts of initial basic magma give important information on the origin and evolution of granitic magmas. The mafic microgranular enclaves from the l-type Kozak pluton are less than...
Geology and Hydrothermal Alteration of the Aydın-Salavatlı Geothermal Field, Western Anatolia, Turkey
geothermal field hydrothermal alteration Büyük Menderes Graben Salavatlı western Anatolia Turkey
2009/7/8
The Aydın-Salavatlı geothermal field is located in the middle part of the Büyük Menderes Graben, and is characterized by normal-fault structures. The stratigraphic sequence of the Aydın...
The Problem of the Core-Cover Boundary of the Menderes Massif and an Emplacement Mechanism for Regionally Extensive Gneissic Granites, Western Anatolia (Turkey)
gneissic granites syntectonic granites Menderes Massif western Anatolia
2009/7/8
In previous studies, the stratigraphy of the Menderes Massif was divided into a Precambrian core and Mesozoic cover associations, the core consisting of gneissic granites and high-grade schists and th...
Halitpaşa Transpressive Zone: Implications for an Early Pliocene Compressional Phase in Central Western Anatolia, Turkey
western Turkey Aegean Late Cenozoic transpression extension
2009/7/8
The Late Cenozoic evolution of the eastern Aegean is dominated by widespread continental extension. The most prominent structures are E-W- and NE-SW-trending grabens and intervening horsts, while NW-...
Geotectonic Setting and Origin of the Youngest Kula Volcanics (Western Anatolia), with a New Emplacement Model
western Anatolia extensional tectonics Kula volcanics geochemistry
2009/7/7
The Quaternary Kula volcanics are Na-dominant in character while all the older volcanic rocks of western Anatolia are generally definitive K-dominant rocks. As a unique example in western Anatolia, th...
Stratigraphic and Palaeoenvironmental Significance of Bartonian–Priabonian (Middle–Late Eocene) Microfossils from the Başçeşme Formation, Denizli Province, Western Anatolia
Middle-Late Eocene mangrove western Anatolia benthic foraminifer palynomorph palaeoenvironment palaeoclimate
2009/7/7
This study explains the stratigraphical and palaeoenvironmental significance of Bartonian-Priabonian (Middle-Late Eocene) fossils, the fauna and flora obtained from the Başçeşme forma...
Petrography and Geochemistry of Paragneisses in the Çine Submassif of the Menderes Massif, Western Anatolia
paragneiss geochemistry metamorphism Menderes Massif western Anatolia
2009/7/7
The Menderes Massif, which covers a large area in western Turkey, is made up of Pan-African basement rocks and a Palaeozoic to Early Tertiary cover sequence. The study area is located in the Dalama an...
Stratigraphy and Geochemical Features of the Early Miocene Bimodal (Ultrapotassic and Calc-alkaline) Volcanic Activity Within the NE-trending Selendi Basin, Western Anatolia, Turkey
Western Anatolia lamproite ultrapotassic volcanism bimodal volcanism continental extension
2009/7/7
Western Anatolia has experienced thickening and orogenic collapse subsequent to the Eocene continent-arc collision. The early stage of the post-collisional volcanism in the region was thought to have...
Stratigraphic and Structural Evidence for Fault Reactivation: The Active Manisa Fault Zone, Western Anatolia
Manisa fault zone active fault relay ramp reactivation west Anatolia
2009/7/7
In this paper, we aim to present stratigraphic and structural evidence for fault reactivation that is linked with evolution of the western part of the Manisa fault zone - a major range-bounding fault ...
A First Record of a Strike-slip Basin in Western Anatolia and Its Tectonic Implication: The Cumaovası Basin
Cumaovası strike-slip basin transpression transtension extension western Anatolia
2009/7/7
The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western end of Gediz and Küçük Menderes grabens in the west Anatolian extensional province. It i...
Isostatic Compensation in Western Anatolia with Estimate of the Effective Elastic Thickness
effective elastic thickness isostatic response functions gravity Western Anatolia admittance analysis
2009/7/7
Isostasy is concerned with how the crust and mantle adjusts to shifting loads of limited spatial and temporal dimensions. By analysing the frequency content of gravity and topography data, it has been...
Statistical Earthquake Frequency Analysis for Western Anatolia
extreme value distribution Western Anatolia zonation seismic assessment earthquake
2009/7/7
In order to apply a statistical earthquake frequency analysis to western Anatolia, the area has been restricted within coordinates 36.50º-40º North and 26.00º-30.00º East. Data use...
Empirical Attenuation Relationships for Western Anatolia,Turkey
attenuation relationship horizontal-to-vertical spectral ratio peak ground acceleration nonlinear soil behaviour western Anatolia Turkey
2010/1/11
Seismic hazard studies have become progressively more important for earthquake engineering applications in western Anatolia, which contains one of the world’s best examples of a rapidly extending intr...