Önemli Makaleler

<html lang="en"> <head><meta charset="utf-8" /><meta http-equiv="X-UA-Compatible" content="IE=edge" /><meta name="viewport" content="width=device-width, initial-scale=1, shrink-to-fit=no" /><title> Önemli Makaleler </title><link href="https://fonts.googleapis.com/css?family=Source+Sans+Pro:300,400,600,700,900&subset=latin-ext" rel="stylesheet" /><link rel="stylesheet" href="/Sitefinity/WebsiteTemplates/MozaikV3/App_Themes/MozaikV3Template/Assets/css/bundle-layout.min.css" /> <script src="/Sitefinity/WebsiteTemplates/MozaikV3/App_Themes/MozaikV3Template/Assets/js/bundle-main.min.js"></script> <link rel="stylesheet" href="/Sitefinity/WebsiteTemplates/MozaikV3/App_Themes/MozaikV3Template/custom/css/style.css" /><meta property="og:title" content="Önemli Makaleler" /><meta property="og:url" content="https://eies.itu.edu.tr/arastirma/onemli-makaleler" /><meta property="og:type" content="website" /><meta property="og:site_name" content="Avrasya Yer Bilimleri Enstitüsü" /><meta 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border-style: none; transform: scale(1); transition: transform .9s; opacity: 1; -webkit-filter: grayscale(100%); /* Safari 6.0 - 9.0 */ filter: grayscale(100%); } .img-full img:hover { transform:scale(1.12); transition: transform .9s; opacity: 0.8; -webkit-filter: none; /* Safari 6.0 - 9.0 */ filter: none; } } .teachers-area.section-padding { padding-bottom: 70px; } .agent { box-shadow: 0 0 10px rgba(0, 0, 0, 0.1); -webkit-transition: all 0.3s ease 0s; transition: all 0.3s ease 0s; } .agent .image { position: relative; overflow: hidden; } .agent .image .img { display: block; } .agent .image .social { position: absolute; top: 50%; -webkit-transform: translateY(-50%); transform: translateY(-50%); left: 15px; } .agent .image .social a { width: 30px; height: 30px; padding: 5px; text-align: center; border-radius: 50px; display: block; color: #ffffff; margin-bottom: 5px; margin-left: -50px; } .agent:hover .image .social a { margin-left: 0; } .agent .image .social a:hover { opacity: 0.9; -ms-filter: "progid:DXImageTransform.Microsoft.Alpha(Opacity=90)"; } .agent .image .social a.facebook { background-color: #4867AA; } .agent .image .social a:nth-child(2) { -webkit-transition-delay: 0.15s; transition-delay: 0.15s; } .agent .image .social a.twitter { background-color: #1DA1F2; } .agent .image .social a:nth-child(3) { -webkit-transition-delay: 0.3s; transition-delay: 0.3s; } .agent .image .social a.linkedin { background-color: #007BB6; } .agent .image .social a:nth-child(4) { -webkit-transition-delay: 0.45s; transition-delay: 0.45s; } .agent .image .social a.google { background-color: #DD5144; } .agent .image .social a i { display: block; font-size: 14px; line-height: 20px; } .agent .content { display: -webkit-box; display: -ms-flexbox; display: flex; -webkit-box-orient: vertical; -webkit-box-direction: normal; -ms-flex-direction: column; flex-direction: column; text-align: left; padding: 20px; background-color: #f7f7f7; } .agent .content .title { font-weight: 400; margin-bottom: 10px; font-size: 16px; } .agent .content .title a { color: #000; } .agent .content .phone, .agent .content .email { line-height: 20px; margin-bottom: 5px; } .agent .content .properties { font-size: 13px; line-height: 18px; color: #004395; font-weight: 500; margin-top: 5px; } /* ------- Eğitmenlerimiz-------- */ /* ------- Eğitmenlerimiz Detay -------- */ .mb-30 { margin-bottom: 30px; } @media (min-width: 992px){ .col-lg-5 { -webkit-box-flex: 0; -ms-flex: 0 0 41.666667%; flex: 0 0 41.666667%; max-width: 41.666667%; } } @media (min-width: 992px){ .col-lg-7 { -webkit-box-flex: 0; -ms-flex: 0 0 58.333333%; flex: 0 0 58.333333%; max-width: 58.333333%; } } .team-image img { width: 100%; } .team-content .title { margin-bottom: 15px; font-weight: 600; font-size: 24px; } .team-content p { margin-bottom: 25px; } .team-content h4 { font-size: 18px; margin-bottom: 15px; font-weight: 600; } .team-content ul li { color: #666666; display: -webkit-box; display: -ms-flexbox; display: 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.social a { width: 30px; height: 30px; padding: 5px; text-align: center; border-radius: 50px; display: block; color: #ffffff; margin-right: 10px; } .social a:last-child { margin-right: 0; } .social a:hover { opacity: 0.9; } .social a i { display: block; font-size: 14px; line-height: 20px; } .social a.facebook { background-color: #4867AA; } .social a.twitter { background-color: #1DA1F2; } .social a.linkedin { background-color: #007BB6; } .social a.google { background-color: #DD5144; } .social a.instagram { background-color: #B23A94; } .social a.pinterest { background-color: #BD081B; } .social a.skype { background-color: #00A9F0; } .social a.tumblr { background-color: #36465D; } .social a:nth-child(2) { -webkit-transition-delay: 0.15s; -o-transition-delay: 0.15s; transition-delay: 0.15s; } .social a:nth-child(3) { -webkit-transition-delay: 0.3s; -o-transition-delay: 0.3s; transition-delay: 0.3s; } .social a:nth-child(4) { -webkit-transition-delay: 0.45s; -o-transition-delay: 0.45s; transition-delay: 0.45s; } .social a:nth-child(5) { -webkit-transition-delay: 0.6s; -o-transition-delay: 0.6s; transition-delay: 0.6s; } .social a:nth-child(6) { -webkit-transition-delay: 0.75s; -o-transition-delay: 0.75s; transition-delay: 0.75s; } .social a:nth-child(7) { -webkit-transition-delay: 0.9s; -o-transition-delay: 0.9s; transition-delay: 0.9s; } .social a:nth-child(8) { -webkit-transition-delay: 1.05s; -o-transition-delay: 1.05s; transition-delay: 1.05s; } /* ------- Eğitmenlerimiz Detay -------- */</style></head> <body> <form method="post" action="./onemli-makaleler" id="form1"> <div class="aspNetHidden"> <input type="hidden" name="ctl08_TSM" id="ctl08_TSM" value="" /> <input type="hidden" name="ctl09_TSSM" id="ctl09_TSSM" value="" /> <input type="hidden" name="__EVENTTARGET" id="__EVENTTARGET" value="" /> <input type="hidden" name="__EVENTARGUMENT" id="__EVENTARGUMENT" value="" /> <input type="hidden" name="__VIEWSTATE" id="__VIEWSTATE" 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id="ctl00_cphpageTitle_T44395CC8009_ctl00_ctl00_Breadcrumb" class="RadSiteMap RadSiteMap_Default"> <ul class="rsmFlow rsmLevel rsmOneLevel"> <li class="rsmItem sfBreadcrumbNavigation"><a class="rsmLink" href="../anasayfa">Anasayfa</a><span class='sfBreadcrumbNodeSeparator'>/</span></li> <li class="rsmItem sfNoBreadcrumbNavigation"><a class="rsmLink" href="javascript: void(0)">Önemli Makaleler</a></li> </ul><input id="ctl00_cphpageTitle_T44395CC8009_ctl00_ctl00_Breadcrumb_ClientState" name="ctl00_cphpageTitle_T44395CC8009_ctl00_ctl00_Breadcrumb_ClientState" type="hidden" /> </div> </div> </div> </div> </div>  <div class="main-container">     <div class="content-area"> <div class="row"> <div class='sfContentBlock'><hr /> <h3><span style="font-size: 24px;">İKLİM VE DENİZ BİLİMLERİ ABD</span></h3> <hr /> <h3>Dr. Öğr. Üyesi Nazlı Olğun Kıyak</h3> <ul> <li><span style="font-size: 14px;"><strong>Olgun N., </strong>Tarı U., Balcı N., Altunkaynak Ş., Gürarslan I., Deniz Yakan S., Thalasso F., Astargo-Espana M.S, Cabrol L., Lavargne C., Hoffmann L., 2024. Lithological controls on lake water biogeochemistry in Maritime Antarctica. Science of the Total Environment, 912, 168562.</span></li> </ul> <h3> <br /> Dr. Öğr. Üyesi Ömer Yetemen</h3> <ul> <li>Istanbulluoglu, E.,<strong> O. Yetemen,</strong> E.R. Vivoni, H.A. Gutierrez-Jurado and R.L. Bras (2008). Eco-geomorphic implications of hillslope aspect: Inferences from analysis of landscape morphology in central New Mexico, Geophysical Research Letters, 35, L14403.</li> </ul> <ul> <li>Kumari, N., P.M. Saco, J.F. Rodriguez, S.A. Johnstone, A. Srivastava, K.P. Chun, and <strong>O. Yetemen </strong>(2020). The grass is not always greener on the other side: Seasonal reversal of vegetation greenness in aspect-driven semiarid ecosystems. Geophysical Research Letters, 47(15), e2020GL088918.</li> </ul> <ul> <li><strong><strong>Yetemen, </strong>O.,</strong> Saco, P.M., Istanbulluoglu, E. (2019). Ecohydrology controls the geomorphic response to climate change. Geophysical Research Letters, 46(15), 8852-8861.</li> </ul> <ul> <li> <strong>Yetemen, O.</strong>, E. Istanbulluoglu and A.R. Duvall (2015). Solar radiation as a global driver of hillslope asymmetry: Insights from an ecogeomorphic landscape evolution model. Water Resources Research, 51, 9843-9861.</li> </ul> <ul> <li> <strong>Yetemen, O.</strong>, E. Istanbulluoglu, J.H. Flores-Cervantes, E.R. Vivoni and R.L.Bras (2015). Ecohydrologic role of solar radiation on landscape evolution. Water Resources Research, 51, 1127-1157.</li> </ul> </div><div class='sfContentBlock'><hr /> <h3><span style="font-size: 24px;">KATI YER BİLİMLERİ ABD</span></h3> <hr /> <h3><span style="font-size: 20px;">Prof. Dr. Hans Jensen Thybo<br /> </span></h3> <ul> <li>Artemieva, I.M., <span style="text-decoration: underline;"><strong>Thybo, H.</strong></span>, Shulgin, A., 2016. Geophysical constraints on geodynamic processes at convergent margins: A global perspective. Gondwana Research, 33, 4-23, doi: 10.1016/j.gr.2015.06.010</li> <li>Yang, H., Chemia, C., Artemieva, I.M., and <span style="text-decoration: underline;"><strong>Thybo, H.</strong>,</span> 2017. Control on off-rift magmatism: A case study of the Baikal Rift Zone, Earth Plan. Sci. Lett., <strong>482</strong>, 501-509, doi: 10.1016/j.epsl.2017.11.040</li> <li><span style="text-decoration: underline;"><strong>Thybo, H</strong></span><strong>.</strong> & Artemieva, I. M., 2013, Moho and magmatic underplating in continental lithosphere. Tectonophysics, doi:10.1016/j.tecto.2013.1005.1032.</li> <li><span style="text-decoration: underline;"><strong>Thybo</strong></span><strong>, H.</strong> and C.A. Nielsen, 2009, Magma-compensated crustal thinning in continental rift zones. Nature, doi:10.1038/nature07688.</li> <li><span style="text-decoration: underline;"><strong>Thybo, H.</strong></span>, 2006, The heterogeneous Upper Mantle Low Velocity Zone, <em>Tectonophysics</em>, 416, 53-79.</li> </ul> <hr /> <h3><span style="font-size: 20px;">Prof. Dr. Tahsin Attila Çiner</span></h3> <ul> <li><strong>Çiner, A</strong>., Deynoux, M., Ricou, S., Koşun, E. (1996). Cyclicity in the middle Eocene Çayraz carbonate formation, Haymana Basin, Central Anatolia, Turkey. <em>Paleogeog, Paleoclim, Paleoecol</em>, 121, 3-4, 313-329.</li> <li><strong>Çiner, A</strong>., Koşun, E., Deynoux, M. (2002). Fluvial, evaporitic and shallow marine facies architecture, depositional evolution and cyclicity in the Sivas Basin (Miocene), Central Turkey. <em>J. of Asian Earth Sciences</em>, 2, 147-165.</li> <li><strong>Çiner, A.,</strong> Sarıkaya, M.A., Yıldırım, C. (2015). Late Pleistocene piedmont glaciations in the Eastern Mediterranean; insights from cosmogenic <sup>36</sup>Cl dating of hummocky moraines in southern Turkey.<strong><em></em></strong><em>Quaternary Science Reviews</em>, 116. 44-56. doi:10.1016/j.quascirev.2015.03.017</li> <li><strong>Çiner, A.,</strong> Doğan, U., Yıldırım, C., Akçar, N., Ivy-Ochs, S., Alfimov, V., Kubik,<sup> </sup>P.W., Schlüchter, C. (2015). Quaternary uplift rates of the Central Anatolian Plateau, Turkey: Insights from cosmogenic isochron-burial nuclide dating of the Kızılırmak River terraces. <em>Quaternary Science Reviews</em>, 107, 81-97. doi:10.1016/j.quascirev.2014.10.007</li> <li><strong>Çiner, A., </strong>Yıldırım, C., Sarıkaya, M.A., Seong, Y.B., Byung, Y.Y. (2019).<sup> 10</sup>Be cosmogenic dating of glacial erratic boulders on Horseshoe Island in western Antarctic Peninsula confirm the rapid deglaciation in Early Holocene. <em>Antarctic Science</em>, 31, 6, 319-331. doi:10.1017/S0954102019000439</li> </ul> <hr /> <h3><span style="font-size: 20px;">Doç.Dr. Orkan Özcan</span></h3> <ul> <li><strong>Özcan, O., </strong> & Özcan, O., (2021). Automated UAV based multi-hazard assessment system for bridges crossing seasonal rivers. Smart Structures and Systems, vol.27, no.1, 35-52.     </li> <li>Akay, S. S. , <strong>Özcan, O.,</strong> Sanli, F. B. , Görüm, T., Şen, Ö. L. , & Bayram, B., (2020). UAV-based evaluation of morphological changes induced by extreme rainfall events in meandering rivers. Plos One, vol.15, no.11.</li> </ul> <h3></h3> <hr /> <h3><span style="font-size: 20px;">Dr. Öğr. Üyesi Ali Mohammedi</span></h3> <ul> <li><strong>Mohammadi, A.</strong>, Burg, J-P., Guillong, M., Quadt, A. (2017). Arc magmatism witnessed by detrital zircon U-Pb geochronology, Hf isotopes and provenance analysis of Late Cretaceous-Miocene sandstones of onshore western Makran (SE Iran). American Journal of Science, Vol. 317(8), p. 941-964. Doi:10.2475/08.2017.03</li> <li><strong>Mohammadi, A.</strong>, Burg, J-P., Winkler, W. (2016). Detrital zircon and provenance analysis of Eocene-Oligocene strata in the South Sistan Suture Zone, SE Iran: implications on the tectonic setting. Lithosphere, Vol. 8(6), p. 615-632. Doi:10.1130/L538.1</li> <li><strong>Mohammadi, A.</strong>, Burg, J-P., Winkler, W., Ruh, J., Quadt, A. (2016). Detrital zircon and provenance analysis of Late Cretaceous-Miocene onshore Iranian Makran strata: implications on the tectonic setting. Geological Society of America Bulletin, Vol. 128(9-10), p. 1481-1499. Doi:10.1130/B31361.1</li> <li><strong>Mohammadi, A.</strong>, Burg, J-P., Bouilhol, P., Ruh, J. (2016). U-Pb geochronology and geochemistry of Zahedan and Shah Kuh plutons, southeast Iran: Implication for closure of the South Sistan Suture Zone. Lithos, Vol. 248, p. 293-308. Doi.org/10.1016/j.lithos.2016.02.003</li> <li>Ruh, J., Hirt, A., Burg, J-P., <strong>Mohammadi, A.</strong> (2014). Forward propagation of the Zagros Simply Folded Belt constrained from magnetostratigraphy of growth strata. Tectonics,<em> </em>Vol. 33(8),<em> </em>p. 1534-1551. Doi.org/10.1002/2013TC003465 </li> </ul> <hr /> <h3><span style="font-size: 20px;">Dr. Öğr. Üyesi Georg Johannes Schwamborn</span></h3> <ul> <li style="text-align: left;">Mohammadi, A., Lak, R., <strong>Schwamborn, G.,</strong> Firouz, A. K., Çiner, A., & Khatouni, J. D. (2021). Depositional environments and salt-thickness variations in Urmia Lake (NW Iran): Insight from sediment-core studies. Journal of Sedimentary Research, 91(3), 296-316. doi.org/10.2110/jsr.2020.078</li> <li style="text-align: left;"><strong>Schwamborn, G.,</strong> Manthey, C., Diekmann, B., Raschke, U., Zhuravlev, A., Prokopiev, A. V., & Schirrmeister, L. (2020). Late Quaternary sedimentation dynamics in the Beenchime-Salaatinsky Crater, Northern Yakutia. arktos, 6(1), 75-92. doi.org/10.1007/s41063-020-00077-w</li> <li style="text-align: left;"><strong>Schwamborn, G.,</strong> Hartmann, K., Wünnemann, B., Rösler, W., Wefer-Roehl, A., Pross, J., ... & Diekmann, B. (2020). Sediment history mirrors Pleistocene aridification in the Gobi Desert (Ejina Basin, NW China). Solid Earth, 11(4), 1375-1398. doi.org/10.5194/se-11-1375-2020</li> </ul> <br /> <br /> <p><span style="font-size: 13px;"></span></p> </div> </div> </div> </div>  <div class="footer">    <div class='sfContentBlock'><div class="footer__top"> <div class="container"> <div class="row address"> <div class="col-xs-12 col-md-4"> <div class="address__item"> <em class="icon-phone"></em> <p><strong>Avrasya Yer Bilimleri Enstitüsü - Telefon</strong>0212 285 61 08</p> </div> </div> <div class="col-xs-12 col-md-4"> <div class="address__item"> <em class="icon-fax"></em> <p><strong>Avrasya Yer Bilimleri Enstitüsü - Fax</strong>0212 285 62 10</p> </div> </div> <div class="col-xs-12 col-md-4"> <div class="address__item"> <em class="icon-location"></em> <p><strong>Avrasya Yer Bilimleri Enstitüsü - Adres </strong> İTÜ, Ayazağa Kampüsü, 34469 Maslak / İstanbul</p> </div> </div> </div> </div> </div> </div>   <div class='sfContentBlock'><div class="footer__bottom"> <div class="container"> <div class="row"> <div class="col-xs-12 col-md-4 footer__logo"> <a href="https://www.itu.edu.tr"><img alt="" src="/Sitefinity/WebSiteTemplates/MozaikV3/App_Themes/MozaikV3Template/Assets/images/logo_footer.png" /></a> </div> <div class="col-xs-12 col-md-4 col-md-push-4 footer__social"> <div class="footer__social-list"><a href="https://www.facebook.com/itu1773" target="_blank" class="footer__social-list-item"> <em class="icon-facebook"></em></a> <a href="https://twitter.com/itu1773" target="_blank" class="footer__social-list-item"> <em class="icon-twitter"></em></a> <a href="https://www.youtube.com/itu1773" target="_blank" class="footer__social-list-item"> <em class="icon-youtube"></em></a> <a href="https://www.instagram.com/itu1773/" target="_blank" class="footer__social-list-item"> <em class="icon-instagram"></em></a> <a href="https://www.linkedin.com/school/itu1773" target="_blank" class="footer__social-list-item"><em class="icon-linkedin"></em></a> </div> </div> <div class="col-xs-12 col-md-4 col-md-pull-4 footer__copyright"> <p>İTÜ Bilgi İşlem Daire Başkanlığı © <span id="siteYear"></span></p> </div> </div> </div> </div> </div> </div>  </div> <script type="text/javascript"> //<![CDATA[ window.__TsmHiddenField = $get('ctl08_TSM');//]]> </script> <script type="text/javascript">$(document).ready(function() { var date = new Date(); $("#siteYear").html(date.getFullYear()); });</script> <script type="text/javascript"> //<![CDATA[ ;(function() { function loadHandler() { var hf = $get('ctl09_TSSM'); if (!hf._RSSM_init) { hf._RSSM_init = true; hf.value = ''; } hf.value += ';Telerik.Web.UI, Version=2019.3.917.45, Culture=neutral, PublicKeyToken=121fae78165ba3d4:tr:cb7ecd12-8232-4d4a-979d-f12706320867:580b2269:eb8d8a8e'; Sys.Application.remove_load(loadHandler); }; Sys.Application.add_load(loadHandler); })();Sys.Application.add_init(function() { $create(Telerik.Web.UI.RadSiteMap, null, null, null, $get("ctl00_cphpageTitle_T44395CC8009_ctl00_ctl00_Breadcrumb")); }); //]]> </script> </form> </body> </html>

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