6 research outputs found
Geological, petrological, and geodynamical characteristics of the Karacaali Magmatic Complex (Kirikkale) in the Central Anatolian Crystalline Complex, Turkey
WOS: 000344525100005Mafic and felsic igneous rocks in the Karacaali Magmatic Complex (KMC) in the northwestern margin of the Central Anatolian Crystalline Complex (CACC) are classified into 4 groups: i) granitoid pluton including granite, granodiorite, and monzonite; ii) a few meter-scale porphyritic microgranite enclaves within the hybrid rocks; iii) hybrid rocks formed by mixing/mingling of mafic lavas (basaltic/diabasic/lamprophyric), anorthositic, and/or rhyolitic lavas; iv) diabasic dykes/veins within the granitoid pluton. Major element composition of the granitoid pluton and porphyritic microgranite enclaves within the hybrid rocks indicate subalkaline, calc-alkaline, and mostly I-type characteristics. These rocks are mainly peraluminous with aluminum saturation index > 1, but mainly between 1 and 1.1, indicating transitional peraluminous. On the tectonomagmatic discrimination diagrams (Y vs. Nb and (Y+Nb) vs. Rb diagrams), all the granitic and monzonitic rock suites from the complex fall mostly in the VAG+Syn-COLG and VAG fields respectively, suggesting arc-related origin. On the R1 vs. R2 tectonic diagram, the granitic rocks display distribution from preplate collision to syncollision field, but quartz-monzonitic samples plot within the postcollision uplift field. Based on limited geological, petrographic, and geochemical results, the tectonomagmatic evolution of the KMC can be summarized as follow: i) initiation of subduction of the Inner Tauride oceanic lithosphere beneath the CACC during the Late Cretaceous time; ii) underplating of partial melts derived from subducted slab and/or mantle wedge, which provided enough heat for partial melting of the mafic lower crust and generation of granitic magma; iii) slab detachment following the continent-continent collision that resulted in tensional forces within the overlying continental crust, which allowed the intrusion of the granitic magma to the upper crust, also cutting the central Anatolian ophiolites, from the Late Cretaceous to most likely the Paleocene time. The hybrid rocks formed by mixing/mingling of the mafic, anorthositic, and/or rhyolitic magmas most likely indicate their injection into a partly crystalline granitic magmatic system just after crystallization of granitic magma in the upper crust. However, this model is open to discussion and needs to be investigated using isotope data in future studies
The determination of relations between statistical seismicity data and geodetic strain analysis, and the analysis of seismic hazard in southwest Anatolia
This study aims the relations between seismicity data and strain analysis based on geodetic space techniques in order to define the seismicity hazard of the southwest Anatolian region of Turkey. This region has complex tectonic formations and requires sophisticated techniques and approaches to investigate seismic activities. In this study, global navigation satellite system (GNSS) observations were used to determine the velocity field of the region. The strain rates of the region were obtained from the evaluation of this velocity field. In addition, seismicity b parameters of the region were calculated from the analysis of seismicity data. Furthermore, the seismicity data and the geodetic strain rates obtained from the GNSS observations were combined to show the statistical correlation. This correlation was interpreted to define the seismicity. According to the results derived from the correlation analysis, the geodetic strain analysis and seismicity data were highly and inversely correlated (r = −0.96). After the determination of the correlation, the seismic hazard data of the region was added to the analysis. This process shows that seismic hazards are highly and negatively correlated to seismicity data (r = −0.90), even though they are highly but positively correlated to geodetic strain analysis (r = 0.88)
A 2300-year record of environmental change from SW Anatolia, Lake Burdur, Turkey
International audienc
Impact of vitamin D insufficiency on the epicardial coronary flow velocity and endothelial function
Objective Increasing evidence suggests a relationship between vitamin D (VD) insufficiency and cardiovascular disease. The present study evaluated the effect of VD insufficiency on epicardial coronary flow rate, subclinical atherosclerosis, and endothelial function.Methods The present study was cross-sectional and observational. We enrolled 222 consecutive patients who had undergone coronary angiography for suspected ischemic heart disease and were found to have normal or near-normal coronary arteries. Thereafter, 25(OH)D3 levels were measured and the coronary flow rate was assessed using the thrombolysis in myocardial infarction frame count. Slow coronary flow (SCF) was defined as a thrombolysis in myocardial infarction frame count greater than 27/frame. Endothelial function was assessed by brachial artery flow-mediated dilatation. Carotid intima-media thickness, an indicator of subclinical atherosclerosis, was measured using B-mode ultrasonography.Results The mean level of 25(OH)D3 was 31.8 ng/ml, and 47% (n=106) of the patients had insufficient 25(OH)D levels (<30 ng/ml). Baseline characteristics were similar between VD-insufficient and VD-sufficient groups. The incidence of SCF was significantly higher in the VD-insufficient group than in patients with sufficient VD (relative risk=3.5, 95% confidence interval=1.1-10.5, P=0.01). After adjusting for cardiovascular disease risk factors, VD insufficiency was independently associated with SCF. The linear regression analysis showed that VD insufficiency was correlated independently with % flow-mediated dilatation (=0.424, P<0.001) and carotid intima-media thickness (=0.43, P<0.001).Conclusion A strong association was found between VD insufficiency and the SCF phenomenon. In addition, VD insufficiency was associated with endothelial dysfunction and subclinical atherosclerosis. We believe that further studies are required to clarify the role of VD in patients with SCF
Reproducibility of fluorescent expression from engineered biological constructs in E. coli
We present results of the first large-scale interlaboratory study carried out in synthetic biology, as part of the 2014 and 2015 International Genetically Engineered Machine (iGEM) competitions. Participants at 88 institutions around the world measured fluorescence from three engineered constitutive constructs in E. coli. Few participants were able to measure absolute fluorescence, so data was analyzed in terms of ratios. Precision was strongly related to fluorescent strength, ranging from 1.54-fold standard deviation for the ratio between strong promoters to 5.75-fold for the ratio between the strongest and weakest promoter, and while host strain did not affect expression ratios, choice of instrument did. This result shows that high quantitative precision and reproducibility of results is possible, while at the same time indicating areas needing improved laboratory practices.Peer reviewe