Spatiotemporal variability of precipitation concentration in western Turkey   总被引：1，自引：0，他引：1  

Ercan Yeşilırmak  Levent Atatanır 《Natural Hazards》2016,81(1):687-704

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Trace element composition of rutile and Zr-in-rutile thermometry in meta-ophiolitic rocks from the Kazdağ Massif,NW Turkey     

Fırat Şengün  Thomas Zack 《Mineralogy and Petrology》2016,110(4):547-560

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Late Cretaceous arc igneous activity: the Eğrikar Monzogranite example     

F. Sipahi  A. Kaygusuz  Ç. Saydam Eker  A. Vural  İ. Akpınar 《International Geology Review》2018,60(3):382-400

The geochemical and Sr–Nd–Pb isotope properties, as well as the Laser Ablation Inductively Coupled Plasma and Mass Spectrometry (LA-ICP-MS) U–Pb zircon age, of E?rikar Monzogranite in the eastern Pontides, are primarily investigated in this study with the aim of determining its magma source and geodynamic evolution. The U–Pb zircon age obtained from E?rikar Monzogranite is 78 ± 1.5 Ma, thereby re?ecting the age of monzogranite. The I-type E?rikar Monzogranite comprises quartz, plagioclase (An_35–45), orthoclase, muscovite, and biotite. The geochemical analyses of the E?rikar Monzogranite indicate being medium K calc-alkaline, peraluminous, and resembling magmatic arc granite. The E?rikar Monzogranite is enriched in large ion lithophile elements and light rare earth elements relative to high field strength elements. Chondrite-normalized rare earth element patterns have concave upward shapes (La_N/Yb_N 2.47–8.58) with pronounced negative Eu anomalies (Eu_N/Eu* = 0.29–0.65). Initial εNd_(i) values vary between 1.85 and 2.18 and initial ⁸⁷Sr/⁸⁶Sr values between 0.7048 and 0.7067. Fractionation of plagioclase, hornblende, and apatite played an important role in the evolution of E?rikar Monzogranite. The crystallization temperatures of the melts ranged from 770°C to 919°C based on zircon and apatite saturation temperatures. The geochemical and isotopic data suggest being generated by the partial melting of ma?c lower crustal sources.  相似文献   

Prioritization of hazard profile for Istanbul using Analytical Hierarchy Process     

N. Özeyranlı Ergenç  Ş. Barış 《Natural Hazards》2018,90(1):325-336

The compilation of the data for past disasters is vital for taking lessons from the past, investigating their reasons, preventing the loss in the future and for disaster planning-related works. In Turkey, especially in Istanbul which has a historical background of more than 8000 years, the demand for backdated disaster data increases to determine the dangers that the city is faced with and to analyze them. The purpose of our work is to develop a hazard profile identification model for Istanbul by using “Analytic Hierarchy Process.” Therefore, we searched for different types of disasters and hazard classifications in various national and international databases. We scrutinized the kinds of disasters, hazards and hazard characteristics that should be used for a proposed model. By examining “Istanbul’s 2000 Years of Disaster Database” and 100 years of Republic’s statistics prepared for Istanbul, we identified the disaster categories and criteria, ran the Analytic Hierarchy Process and created a hazard profile model for Istanbul. Consequently, we proved that the most important types of disasters that affect Istanbul are geophysical disasters followed by climatological, hydrological, meteorological and technological disasters. The work also shows us that the districts which have a high rate of the population such as Bagcilar, Kucukcekmece and Esenyurt are more vulnerable to these hazards.  相似文献   

Multipath interference cancelation in GPS time series under changing physical conditions by means of adaptive filtering     

Aydın Üstün  Sefa Yalvaç 《Earth Science Informatics》2018,11(3):359-371

Multipath, a highly autocorrelated signal is observable phenomena during time periods longer than the sidereal period of Global Positioning System (GPS) satellites in their constellations. Multipath pattern and sidereal repeat time interaction are examined in terms of time series correlations of topocentric coordinates using GPS code and phase observations collected at high and low frequencies. The horizontal and vertical components at 5 and 30 s sampling rates are analyzed to detect and remove multipath classified by their M P ₁ levels and baseline lengths. For the selected 11 stations that have 24-hour data from CORS stations in the USA and Turkey, the repeat times of the GPS constellation were identified as a function of maximum cross-correlation of adjacent time series. The multipath interference signal from two-day time series data is removed by an adaptive filter to improve time series of coordinate estimates. After the filtering process, an effective epoch based position tracking has been accomplished, especially in the height component. The position errors disappeared to maximum possible extent in the pseudo-range measurements. Up to 70% improvement for the phase derived coordinates in reflective environment has been achieved over the baselines ranging from 1 km to 175 km. For the phase observables, the filter success directly related to the multipath level which is specific to the station.  相似文献   

Determination of deterioration of the main facade of the Ferit Paşa Cistern by non-destructive techniques (Konya,Turkey)     

İsmail İnce  Ali Bozdağ  M. Bahadır Tosunlar  M. Ergün Hatır  Mustafa Korkanç 《Environmental Earth Sciences》2018,77(11):420

Building stones have long been one of the most widely used construction materials in the world. Building stones used in historical monuments are deteriorated partly or completely depending on the environmental and atmospheric effects. In recent years, non-destructive test methods have been used to assess deterioration of building stones used in historical monuments. Gödene stone is one of the building stones being widely used in the historical buildings in the Konya region, Central Anatolia. The most deterioration effects are observed in the Ferit Pa?a Cistern among the historical structures built with Gödene stone in the region. The aim of this study is to assess the deteriorating effects in the street façade of the Ferit Pa?a Cistern via non-destructive testing methods (Schmidt hardness rebound value, P-wave velocity, humidity measurement and thermal imaging) and create maps of deteriorated features. Turkey’s historic places are integrated to Turkish culture, efforts are made to conserve heritage through rehabilitation. Therefore, this study will help developers and federal managers during the project planning stage by providing technical data.  相似文献   

Adaptation of hurricane risk perception scale to earthquake risk perception and determining the factors affecting women's earthquake risk perception     

Mızrak  Sefa  Özdemir  Ahmet  Aslan  Ramazan 《Natural Hazards》2021,109(3):2241-2259

Natural Hazards - Worldwide studies show that gender is an important variable affecting disaster risk perception and that women have high levels of disaster risk perception. The objective of this...  相似文献   

The porosity of saturated shallow sediments from seismic compressional and shear wave velocities     

Osman Uyanık 《Journal of Applied Geophysics》2011,73(1):16-24

This study devises a new analytical relationship to determine the porosity of water-saturated soils at shallow depth using seismic compressional and shear wave velocities. Seismic refraction surveys together with soil sample collection were performed in selected areas containing water-saturated clay–silt, sand and gravely soils. Classification of clay–silt, sand and gravel dense soils provided the coefficient of experimental equation between the data sets, namely, Poisson's ratio, shear modulus and porosity values. This study presents a new analytical relationship between Poisson's ratio and shear modulus values, which are obtained from seismic velocities and porosity values of water-saturated material computed from water content and grain densities, which are determined by laboratory analysis of disturbed samples. The analytical relationship between data sets indicates that when the shear modulus of water-saturated loose soil increases, porosity decreases logarithmically. If shear modulus increases in dense or solid saturated soils, porosity decreases linearly.  相似文献   

Geohazards rooted from the northern margin of the Sea of Marmara since the late Pleistocene: a review of recent results     

Görür  Naci  Çağatay  M. Namık 《Natural Hazards》2010,54(2):583-603

Natural Hazards - Owing to its special geodynamic setting on the western extension of the North Anatolian Fault (NAF) and oceanographic setting between Mediterranean and the Black Seas, the Sea of...  相似文献   

Origin of anorogenic ‘lamproite-like’ potassic lavas from the Denizli region in Western Anatolia Extensional Province, Turkey     

Kamil Yılmaz 《Mineralogy and Petrology》2010,99(3-4):219-239

The Denizli region of the Western Anatolia Extensional Province (WAEP) includes a typical example of intra-plate potassic magmatism. Lamproite-like K-rich to shoshonitic alkaline rocks erupted in the Upper Miocene-Pliocene in a tensional tectonic setting. The absence of Nb and Ta depletion, low Th/Zr and high Nb/Zr ratios and distinct isotopic values (i.e. low ⁸⁷Sr/⁸⁶Sr, 0.703523–0.703757; high ¹⁴³Nd/¹⁴⁴Nd, 0.512708–0.512784; high ²⁰⁶Pb/²⁰⁴Pb, 19.079–19.227, ²⁰⁷Pb/²⁰⁴Pb, 15.635–15.682, ²⁰⁸Pb/²⁰⁴Pb, 39.144–39.302) mark an anorogenic geochemical signature of the Denizli volcanics. All of the lavas are strongly enriched in large-ion-lithophile elements (e.g. Ba 1,100–2,200 ppm; Sr 1,900–3,100 ppm; Rb 91–295 ppm) and light rare-earth elements (e.g. La_N?=?319–464), with a geochemical affinity to ocean-island basalts and lack of a recognizable subduction signature or any evidence for crustal contamination. The restricted range of isotopic (Sr, Nd, Pb) ratios in both near-primitive (Mg# 66.7–77.2) and more evolved (Mg# 64.6–68.7) members of the Denizli volcanics signify their evolution from an isotopically equilibrated parental mantle source. Their high Dy/Yb and Rb/Sr values also suggest that garnet and phlogopite were present in the mantle source. Their strong EM-II signature, very low Nd model ages (0.44–049 Ga) and isotopic (Sr-Nd-Pb) values analogous to those of the Nyiragongo potassic basanites and kimberlites from the African stable continental settings, suggest that the parental melts that produced the Denizli volcanics are associated with very young and enriched mantle sources, which include both sublithospheric and enriched subcontinental lithospheric mantle melts. Mantle-lithosphere delamination probably played a significant role in the generation of these melts, and could be related to roll-back of the Aegean arc, lithospheric extension and asthenospheric mantle upwelling.  相似文献