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Journal articles on the topic 'Strandjagt'

Author: Grafiati

Published: 28 July 2024

Last updated: 31 July 2025

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1

Valchovski, Hristo, and İbrahim Mete Misirlioğlu. "Murchieona minuscula (Rosa, 1906): first finding from Bulgaria with earthworm diversity and zoogeography of Yıldız (Strandja) Mountain in Turkey and Bulgaria." Turkish Journal of Zoology 41, no. 4 (2016): 731–36. https://doi.org/10.3906/zoo-1605-46.

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Valchovski, Hristo, Misirlioğlu, İbrahim Mete (2017): Murchieona minuscula (Rosa, 1906): first finding from Bulgaria with earthworm diversity and zoogeography of Yıldız (Strandja) Mountain in Turkey and Bulgaria. Turkish Journal of Zoology 41 (4): 731-736, DOI: 10.3906/zoo-1605-46, URL: http://dx.doi.org/10.3906/zoo-1605-46

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2

Natal’in, Boris A., Gürsel Sunal, Erkan Gün, Bo Wang, and Yang Zhiqing. "Precambrian to Early Cretaceous rocks of the Strandja Massif (northwestern Turkey): evolution of a long lasting magmatic arc." Canadian Journal of Earth Sciences 53, no. 11 (2016): 1312–35. http://dx.doi.org/10.1139/cjes-2016-0026.

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The Strandja Massif, northwestern Turkey, forms a link between the Balkan Zone of Bulgaria, which is correlated with the Variscan orogen in Europe, and the Pontides, where Cimmerian structures are prominent. Five fault-bounded tectonic units form the massif structure. (1) The Kırklareli Unit consists of the Paleozoic basement intruded by the Carboniferous to Triassic Kırklareli metagranites. It is unconformably overlain by Permian and Triassic metasediments. (2) The Vize Unit that is made of Neoproterozoic metasediments, which are intruded by Cambrian metagranites, and overlain by the pre-Ordo

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3

Uzunova, Liana. "Trákija és Elláda - határ nélküli világ. Újabb kihívások és lehetőségek." Jelenkori Társadalmi és Gazdasági Folyamatok 5, no. 1-2 (2010): 33–38. http://dx.doi.org/10.14232/jtgf.2010.1-2.33-38.

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The lecture is trying to carry on and expand with practices from new region of Strandja the issues of the Bulgarian-Greek cooperation in the region of the Rhodopes, presented on the II. Regions in Carpathian Basin conference, which took place in Kaposvár on 22-th of May 2009.

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4

Sunal, Gürsel, Boris A. Natal'in, Muharrem Satir, and Erkan Toraman. "Paleozoic magmatic events in the Strandja Massif, NW Turkey." Geodinamica Acta 19, no. 5 (2006): 283–300. http://dx.doi.org/10.3166/ga.19.283-300.

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5

Spassov, Nikolai, Geko Spiridonov, and Grigor Penev. "The discovery of an extinct species: Data for the recent presence of the Lynx (Lynx lynx L.) in Bulgaria and discussion of its status since 1941." Historia naturalis bulgarica 17 (April 15, 2006): 167–76. https://doi.org/10.5281/zenodo.4043570.

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The accumulated data for the possible or probable presence of the lynx (Lynx lynx) in Bulgaria after the date considered as an official extinction of the animal in the country (1941) are discussed. New reliable data for the recent presence of this carnivore are presented proving its existence in the recent mammal fauna of Bulgaria as well as the beginning of a recovery process from North-West. The possible existence of an unknown local population in Strandja region is also discussed.

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6

SUNAL, G., M. SATIR, B. A. NATAL'IN, G. TOPUZ, and O. VONDERSCHMIDT. "Metamorphism and diachronous cooling in a contractional orogen: the Strandja Massif, NW Turkey." Geological Magazine 148, no. 4 (2011): 580–96. http://dx.doi.org/10.1017/s0016756810001020.

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AbstractThe southern part of the Strandja Massif, northern Thrace, Turkey, comprises a basement of various gneisses, micaschists and rare amphibolite, and a cover of metaconglomerate and metasandstone, separated from each other by a pre-metamorphic unconformity. Metamorphic grade decreases from the epidote–amphibolite facies in the south to the albite–epidote–amphibolite/greenschist-facies transition in the north. Estimated P–T conditions are 485–530°C and 0.60–0.80 GPa in the epidote–amphibolite facies domain, and decrease towards the transitional domain between greenschist- and epidote–amphi

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7

OKAY, ARAL I., ERCAN ÖZCAN, AYNUR HAKYEMEZ, MUZAFFER SIYAKO, GÜRSEL SUNAL, and ANDREW R. C. KYLANDER-CLARK. "The Thrace Basin and the Black Sea: the Eocene–Oligocene marine connection." Geological Magazine 156, no. 1 (2017): 39–61. http://dx.doi.org/10.1017/s0016756817000772.

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AbstractThe Late Cretaceous – Recent West Black Sea Basin and the Eocene–Oligocene Thrace Basin are separated by the Strandja arch comprising metamorphic and magmatic rocks. Since Late Cretaceous time the Strandja arch formed a palaeo-high separating the two basins which accumulated clastic sediment of >9 km thickness. During late Eocene – early Oligocene time the marine connection between these basins existed through the Çatalca gap west of Istanbul. The Çatalca gap lies on the damage zone of a major Cretaceous strike-slip fault; it formed a 15 km wide marine gateway, where carbonate-rich

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8

Ohlendorf, Valerie, Marco Marklewitz, Anne Kopp, Stoyan Yordanov, Christian Drosten, and Sandra Junglen. "Huge diversity of phleboviruses in ticks from Strandja Nature Park, Bulgaria." Ticks and Tick-borne Diseases 10, no. 3 (2019): 697–703. http://dx.doi.org/10.1016/j.ttbdis.2019.03.001.

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9

Dimcheva, Vanya, and Maria Karsheva. "Cistus incanus from Strandja Mountain as a Source of Bioactive Antioxidants." Plants 7, no. 1 (2018): 8. http://dx.doi.org/10.3390/plants7010008.

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10

Szopa, Krzysztof, Anna Sałacińska, Ashley P. Gumsley, et al. "Two-Stage Late Jurassic to Early Cretaceous Hydrothermal Activity in the Sakar Unit of Southeastern Bulgaria." Minerals 10, no. 3 (2020): 266. http://dx.doi.org/10.3390/min10030266.

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Southeastern Bulgaria is composed of a variety of rocks from pre-Variscan (ca. 0.3 Ga) to pre-Alpine sensu lato (ca. 0.15 Ga) time. The Sakar Unit in this region comprises a series of granitoids and gneisses formed or metamorphosed during these events. It is cut by a series of post-Variscan hydrothermal veins, yet lacks pervasive Alpine deformation. It thus represents a key unit for detecting potential tectonism associated with the enigmatic Cimmerian Orogenic episode, but limited geochronology has been undertaken on this unit. Here we report age constraints on hydrothermal activity in the Sak

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11

Suc, Jean-Pierre, Hervé Gillet, M. Namik Çağatay, et al. "The region of the Strandja Sill (North Turkey) and the Messinian events." Marine and Petroleum Geology 66 (September 2015): 149–64. http://dx.doi.org/10.1016/j.marpetgeo.2015.01.013.

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12

Elmas, Ali, İsak Yılmaz, Erdinç Yiğitbaş, and Thomas Ullrich. "A Late Jurassic–Early Cretaceous metamorphic core complex, Strandja Massif, NW Turkey." International Journal of Earth Sciences 100, no. 6 (2010): 1251–63. http://dx.doi.org/10.1007/s00531-010-0540-3.

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13

Boev, Zlatozar. "Late Pleistocene Crocuta crocuta spelaea in Bulgaria: distribution and history of research (Carnivora: Hyaenidae)." Lynx new series 51, no. 1 (2021): 19–29. http://dx.doi.org/10.37520/lynx.2020.002.

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The paper summarizes all scattered data from the last 116 years on the distribution of the Late Pleistocene cave hyena in Bulgaria, a part of them unpublished. Data from 24 fossil sites (Middle Pleistocene – Late Pleistocene) in the country are presented. The fossil record in Bulgaria proves the wide distribution of the species in the karst areas of the low-mountain regions of the country. Its Pleistocene localities are concentrated in the Predbalkan Mts. (83%), Strandja Mts. (8%), Western Rhodopes Mts. (4%) and southern Dobruja Plain (4%). They are situated at the altitudes between 136 and 12

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Cattò, Silvia, William Cavazza, Massimiliano Zattin, and Aral I. Okay. "No significant Alpine tectonic overprint on the Cimmerian Strandja Massif (SE Bulgaria and NW Turkey)." International Geology Review 60, no. 4 (2017): 513–29. http://dx.doi.org/10.1080/00206814.2017.1350604.

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NAUMOVA, MARIA, GERGIN BLAGOEV, and CHRISTO DELTSHEV. "Fifty spider species new to the Bulgarian fauna, with a review of some dubious species (Arachnida: Araneae)." Zootaxa 4984, no. 1 (2021): 228–57. http://dx.doi.org/10.11646/zootaxa.4984.1.18.

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This study is a part of an ongoing comprehensive inventory of Bulgarian spiders. A total of fifty spider species belonging to thirteen families are reported for the first time from Bulgaria. Four species are rejected from the Bulgarian spider checklist due to misidentification: Callilepis concolor Simon, 1914, Centromerus capucinus (Simon, 1884), Hoplopholcus labyrinthi (Kulczyński, 1903) and Mansuphantes prope fragilis (Thorell, 1875). Another four species (Drassodes villosus (Thorell, 1856), Entelecara flavipes (Blackwall, 1834), Lepthyphantes notabilis Kulczyński, 1887 and Singa semiatra L.

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Sunal, Gürsel, Muharrem Satir, Boris A. Natal'in, and Erkan Toraman. "Paleotectonic Position of the Strandja Massif and Surrounding Continental Blocks Based on Zircon Pb-Pb Age Studies." International Geology Review 50, no. 6 (2008): 519–45. http://dx.doi.org/10.2747/0020-6814.50.6.519.

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17

Okay, A., M. Satır, O. Tüysüz, S. Akyüz, and F. Chen. "The tectonics of the Strandja Massif: late-Variscan and mid-Mesozoic deformation and metamorphism in the northern Aegean." International Journal of Earth Sciences 90, no. 2 (2000): 217–33. http://dx.doi.org/10.1007/s005310000104.

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18

Boev, Zlatozar. "Past distribution of Ursus arctos in Bulgaria: fossil and subfossil records (Carnivora: Ursidae)." Lynx new series 51, no. 1 (2021): 5–18. http://dx.doi.org/10.37520/lynx.2020.001.

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The paper summarizes numerous scattered data from the last 120 years on the former distribution of the brown bear (Ursus arctos) in Bulgaria. Data from 52 (13 fossil and 39 subfossil) sites (from the Middle Pleistocene to the 19th century AD) are presented. The brown bear former distribution was much wider than the present occurrence. The species range covered the whole territory of the country, including mountain regions, as well as vast lowland and plain landscapes. The geographical, altitudinal and chronological distribution are presented and analyzed. The record from the Kozarnika Cave (1.

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19

Kurosawa, Masanori, Masao Semmoto, and Toru Shibata. "Mineralogical Characterization of Early Bronze Age Pottery from the Svilengrad-Brantiite Site, Southeastern Bulgaria." Minerals 12, no. 1 (2022): 79. http://dx.doi.org/10.3390/min12010079.

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Several pottery sherds from the Svilengrad-Brantiite site, Bulgaria, were mineralogically and petrographically analyzed. The aim was to add information to the very scarce material data available for Early Bronze Age pottery in the southeastern Thrace plain, Bulgaria, in order to examine a possible raw-material source of the pottery. The characterization techniques applied were optical microscopy (OM), petrographic microscopy (PM), scanning electron microscopy coupled with energy dispersive X-ray spectroscopy (SEM-EDS), X-ray fluorescence (XRF) spectroscopy, and X-ray diffraction (XRD). The pot

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20

Spassov, Nikolai, and Ilya Acosta-Pankov. "Dispersal history of the golden jackal (Canis aureus moreoticus Geoffroy, 1835) in Europe and possible causes of its recent population explosion." Biodiversity Data Journal 7 (May 9, 2019): e34825. https://doi.org/10.3897/BDJ.7.e34825.

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Data on the historical distribution of the golden jackal in Europe and its primary habitats are scarce. There are many new data on the population explosion and the rapid spread of the in Europe. However, the main factors for this expansion, the core population and its routes of dispersal, remain controversial or insufficiently studied. This study provides a profound analysis of the history of the jackal's (<i>Canis aureus moreoticus</i> Geoffroy, 1835) occurrence in Europe, the factors limiting or those triggering its expansion on the continent. The analysis shows that the timing of the specie

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21

Karacık, Zekiye, and Okan Tüysüz. "Petrogenesis of the Late Cretaceous Demirköy Igneous Complex in the NW Turkey: Implications for magma genesis in the Strandja Zone." Lithos 114, no. 3-4 (2010): 369–84. http://dx.doi.org/10.1016/j.lithos.2009.09.012.

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22

Palova, Nadezhda, Iskra Yankova, Boyko Neov, Peter Hristov, and Georgi Radoslavov. "Mitochondrial Diversity of the East Balkan Swine (Sus scrofa f. domestica) in South-Eastern Bulgaria." Acta Veterinaria 69, no. 2 (2019): 229–36. http://dx.doi.org/10.2478/acve-2019-0018.

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Abstract The East Balkan Swine (EBS) is the only preserved local swine breed in Bulgaria and one of the few indigenous pig breeds in Europe. The EBS is distributed in the region of Eastern Balkan Mountains and the Strandja Mountain. To reveal the breed’s genetic profile, we analyzed 50 purebred individuals according to mitochondrial DNA (D-loop region, HVR1) and sequence analysis in the Scientific Center of Agriculture (Sredets region) in the country. The obtained results show the presence of four haplotypes: three Asian specific haplotypes (H1, H2, and H3) and the European specific E1a1. The

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23

VALCHOVSKI, Hristo, and İbrahim Mete MISIRLIOĞLU. "Murchieona minuscula (Rosa, 1906): first finding from Bulgaria with earthworm diversity and zoogeography of Yıldız (Strandja) Mountain in Turkey and Bulgaria." TURKISH JOURNAL OF ZOOLOGY 41 (2017): 731–36. http://dx.doi.org/10.3906/zoo-1605-46.

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24

Ülgen, Semih Can, Nalan Lom, Gürsel Sunal, Axel Gerdes, and Ali Mehmet Celâl Şengör. "The Strandja Massif and the İstanbul Zone were once parts of the same palaeotectonic unit: new data from Triassic detrital zircons." Geodinamica Acta 30, no. 1 (2018): 212–24. http://dx.doi.org/10.1080/09853111.2018.1475447.

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25

Yilmaz Şahin, Sabah, Namık Aysal, Yıldırım Güngör, Irena Peytcheva, and Franz Neubauer. "Geochemistry and U–Pb zircon geochronology of metagranites in Istranca (Strandja) Zone, NW Pontides, Turkey: Implications for the geodynamic evolution of Cadomian orogeny." Gondwana Research 26, no. 2 (2014): 755–71. http://dx.doi.org/10.1016/j.gr.2013.07.011.

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26

MACHEV, Philip, Valentin GANEV, and Laslo KLAIN. "New LA-ICP-MS U-Pb zircon dating for Strandja granitoids (SE Bulgaria): evidence for two-stage late Variscan magmatism in the internal Balkanides." TURKISH JOURNAL OF EARTH SCIENCES 24 (2015): 230–48. http://dx.doi.org/10.3906/yer-1407-21.

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27

Karacık, Zekiye, and Okan Tüysüz. "Corrigendum to “Petrogenesis of the Late Cretaceous Demirköy Igneous Complex in the NW Turkey: Implications for magma genesis in the Strandja Zone” [Lithos 114 (2010), 369–384]." Lithos 117, no. 1-4 (2010): 331. http://dx.doi.org/10.1016/j.lithos.2010.03.010.

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28

Vassileff, Ljuben, and Girgina Stanisheva-Vassileva. "Petrochemical and geodynamic correlation of the porphyry-copper systems in the Eurasian copper belt: the segment Romania – Pakistan." Geologica Balcanica 21, no. 3 (1991): 3.—33. http://dx.doi.org/10.52321/geolbalc.21.3.3.

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The porphyry-copper systems are represented by ore-bearing magmatic complexes which to a greater or lesser extent are the host rocks of mineralization, and the processes involved in the differential formation of intrusive and subvolcanic bodies are similar to those leading to the release and concentration of useful components during some of the subsequent postmagmatic processes. Producers of porphyry-copper ore are mostly the intermediate and slightly acid rocks, the majority showing some tendency towards increased potassic alkalinity. The magmatic systems involved usually manifest several pul

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29

Цанева, Еля. "НЯКОИ ПРЕДВАРИТЕЛНИ БЕЛЕЖКИ КЪМ ПРОБЛЕМИТЕ НА СОЦИО- КУЛТУРНАТА ДИНАМИКА И УСТОЙЧИВОТО РАЗВИТИЕ". Терени, № 4 (18 червня 2025): 3–18. https://doi.org/10.60053/ter.2019.4.3-18.

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The presentation investigates comparatively three critical events in South-East Bulgaria (area of Strandja mountain) in the second decade of the millennium, when the region was struck by particularly critical outbreaks of contagious livestock diseases: foot-and-mouth disease (FMD in 2011), “blue tongue” disease (in 2013), and highly contagious sheep and goat plague (PPR - Peste des Petits Ruminants, in 2018). As well known, in the past local traditional culture responded to the challenges of biological and other hazards through building an adaptive strategy at the edge of rational and spiritua

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30

Sałacińska, Anna, Ianko Gerdjikov, Ashley Gumsley, et al. "Two stages of Late Carboniferous to Triassic magmatism in the Strandja Zone of Bulgaria and Turkey." Geological Magazine, July 21, 2021, 1–14. http://dx.doi.org/10.1017/s0016756821000650.

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Abstract Although Variscan terranes have been documented from the Balkans to the Caucasus, the southeastern portion of the Variscan Belt is not well understood. The Strandja Zone along the border between Bulgaria and Turkey encompasses one such terrane linking the Balkanides and the Pontides. However, the evolution of this terrane, and the Late Carboniferous to Triassic granitoids within it, is poorly resolved. Here we present laser ablation – inductively coupled plasma – mass spectrometry (LA-ICP-MS) U–Pb zircon ages, coupled with petrography and geochemistry from the Izvorovo Pluton within t

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Palandačić, Anja, Oleg A. Diripasko, Sandra Kirchner, Tihomir Stefanov, and Nina G. Bogutskaya. "An integrative approach highlights the discrepancy in the genetic, phenotypic, and presumptive taxonomic structure of Phoxinus (Actinopterygii, Leuciscidae, Phoxininae) in Bulgaria." Journal of Fish Biology, May 6, 2024. http://dx.doi.org/10.1111/jfb.15765.

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AbstractThe present drainage network of Bulgaria is the result of a complex Neogene and Quaternary evolution. Karst, which has developed on 23% of the territory, further complicates the hydrological pattern. Fresh waters of Bulgaria drain into the Black Sea and the Aegean Sea basins and can be roughly divided into the Danube (Middle and Lower Danube), non‐Danube Black Sea, East Aegean, and West Aegean hydrological regions. Phoxinus, a small leuciscid fish, has a mosaic distribution in all four of these regions, inhabiting small mountainous and semi‐mountainous streams. Based on morphology, it

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32

Kounov, Alexandre, Ianko Gerdjikov, Anna Gumsley, et al. "On the presence of a Variscan metamorphism and deformation in the Sakar Unit of Strandja Massif." Review of the Bulgarian Geological Society 85, no. 3 (2024). https://doi.org/10.52215/rev.bgs.2024.85.3.27.

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Here we present the results from several studies confirming the existence of Variscan metamorphic and deformational events in the Sakar Unit of the Strandja Massif. Structural observations and new U-Pb geochronological data from the Mladinovo Complex confirm the existence of migmatisation and high-temperature shearing at 327 ± 2 Ma. The new geochronological data indicate similarities with basement of the Sredna Gora Zone, and it is interpreted that they were both part of the Variscan orogenic belt.

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Akgündüz, Serdar, and Hayrettin Koral. "Paleogene extension in the Northern Aegean: Colluvial/debris flow deposits of the Early-Middle Eocene in NW Thrace Basin, Turkey." Geologica Carpathica 72, no. 3 (2021). http://dx.doi.org/10.31577/geolcarp.72.3.3.

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The Thrace Basin consists of Paleogene–Neogene deposits that lie in the lowland south of the Strandja highlands in NW Turkey, where metagranitic and metasedimentary rocks occur. The Akalan Formation consisting of colluvial fan/debris flow deposits represents the base of the sequence in the northern Thrace basin where it is bounded by a right lateral strike-slip oblique fault called “The Western Strandja Fault Zone”. This formation exhibits a coarse-grained, angular and grain-supported character close to the fault zone which has releasing-bends. Fine-grained, rounded, and matrix-supported sedim

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Ulusoy, Ezgi, and Yusuf Kağan Kadıoğlu. "Petrogenesis of the Late Cretaceous intrusive series in the Strandja Massif, Kırklareli-Türkiye." Geochemistry, December 2024, 126221. https://doi.org/10.1016/j.chemer.2024.126221.

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Yılmaz, Emine. "The Effect of Wild Mushroom Collection in The Mountains of Strandja on The Economic Development of The People Living in The Region." Tekirdağ Ziraat Fakültesi Dergisi, September 3, 2023. http://dx.doi.org/10.33462/jotaf.1332016.

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There is a need for innovative approaches that can accommodate the rural population and manage to keep the rural population in the settlement. At this point, it is important to carry out actions that will adequately meet the living conditions of rural areas and to increase the income levels of rural people. The protection of forests and the maintenance of biological diversity are important in terms of non-wood forest products collected from the forests by the villagers living in that region, and it is very important for the sustainability and economic future of life in the region. In this stud

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V, Dimcheva, and Kursheva M. "Extraction Evaluation of Antioxidant Constituents of Phillyrea Latifolia L. (Wild Olive) from Strandja Mountain, Bulgaria." SunText Review of BioTechnology 01, no. 01 (2020). http://dx.doi.org/10.51737/2766-5097.2020.006.

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Vladinova, Tzvetomila, and Milena Georgieva. "Metamorphism of the westernmost Triassic metasedimentary rocks in the Sakar unit, Sakar–Strandja zone, Bulgaria." Geologica Carpathica 73, no. 4 (2022). http://dx.doi.org/10.31577/geolcarp.73.4.4.

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38

Spassov, Nikolai, and Ilya Acosta-Pankov. "Dispersal history of the golden jackal (Canis aureus moreoticus Geoffroy, 1835) in Europe and possible causes of its recent population explosion." Biodiversity Data Journal 7 (May 9, 2019). http://dx.doi.org/10.3897/bdj.7.e34825.

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Data on the historical distribution of the golden jackal in Europe and its primary habitats are scarce. There are many new data on the population explosion and the rapid spread of the in Europe. However, the main factors for this expansion, the core population and its routes of dispersal, remain controversial or insufficiently studied. This study provides a profound analysis of the history of the jackal’s (Canisaureusmoreoticus Geoffroy, 1835) occurrence in Europe, the factors limiting or those triggering its expansion on the continent. The analysis shows that the timing of the species appeara

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39

ULUSOY, Ezgi, and Yusuf Kağan KADIOĞLU. "The importance of Confocal Raman Spectroscopy and mineral chemistry studies in the magma crystallization processes: Strandja Intrusives, NW Turkey." Bulletin Of The Mineral Research and Exploration, May 13, 2022, 1–18. http://dx.doi.org/10.19111/bulletinofmre.1116573.

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40

ALTINIŞIK, İlkay, and Deniz YAĞLIOĞLU. "Age and Growth of the Bulgarian Minnow, Phoxinus strandjae (Drensky, 1926) (Actinopterygii: Cypriniformes: Cyprinidae) Living in Melen River Basin (Düzce, Turkey)." Natural and Engineering Sciences, April 4, 2022, 39–47. http://dx.doi.org/10.28978/nesciences.1098664.

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41

NATALIN, BORIS, GÜRSEL SUNAL, MUHARREM SATIR, and ERKAN TORAMAN. "Tectonics of the Strandja Massif, NW Turkey: History of a Long-Lived Arc at the Northern Margin of Palaeo-Tethys." Turkish Journal of Earth Sciences, January 1, 2012. http://dx.doi.org/10.3906/yer-1006-29.

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42

Nader, Julian, Nina Król, Martin Pfeffer, et al. "The diversity of tick-borne bacteria and parasites in ticks collected from the Strandja Nature Park in south-eastern Bulgaria." Parasites & Vectors 11, no. 1 (2018). http://dx.doi.org/10.1186/s13071-018-2721-z.

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43

Sałacińska, Anna, Ianko Gerdjikov, Alexandre Kounov, et al. "Variscan magmatic evolution of the Strandja Zone (Southeast Bulgaria and Northwest Turkey) and its relationship to other North Gondwanan margin terranes." Gondwana Research, April 2022. http://dx.doi.org/10.1016/j.gr.2022.04.013.

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Akgündüz, Serdar, Namik Aysal, Irena Peytcheva, Sabah Yilmaz Şahin, and Yildirim Güngör. "Geochronology, geochemistry and tectono-magmatic evolution of the upper Carboniferous–lower Permian Kula pluton in the Istranca (Strandja) Massif, NW Turkey." Geologica Carpathica 72, no. 5 (2021). http://dx.doi.org/10.31577/geolcarp.72.5.2.

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Sezen, Ebru, and Zehra Karakaş. "Newly identified uranyl vanadate mineral formation in the Thrace Basin, NW Türkiye: Insights into identification and origin of carnotite and tyuyamunite minerals." Bulletin Of The Mineral Research and Exploration, September 23, 2024, 1–2. http://dx.doi.org/10.19111/bulletinofmre.1554734.

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The Thrace Basin is located in the northwest of Türkiye, bounded by the Rhodope Zones to the west, the Strandja (Istranca, Strandzha) Massif to the North, and the İstanbul Zone to the east. The Stranja Massif’s basement is composed of the Tekedere Group, which includes Paleozoic gneisses and schists, as well as the Şeytandere Metagranite, consisting of altered and unaltered metagranites. Unaltered metagranites are characterized by large feldspar crystals and are typically white and pink in color, while altered metagranites are typically yellow color. The subject of this study Şeytandere metagr

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Zulauf, G., W. Dörr, R. Albert, S. O. Martha, and P. Xypolias. "Provenance of far-traveled nappes in the eastern Mediterranean (Uppermost Unit, Crete): constraints from U–Pb zircon ages of detrital and igneous zircons." International Journal of Earth Sciences, November 4, 2023. http://dx.doi.org/10.1007/s00531-023-02356-9.

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AbstractNew U–Pb ages of detrital and igneous zircons of the Uppermost Unit of Crete shed light on its provenance and on Eohellenic to Eoalpine imprints in the eastern Mediterranean. The detrital zircons of all nappes show Variscan ages and are characterized by a Minoan-type age spectrum, which is typical for the NE margin of Gondwana. Parts of the metasedimentary rocks are unexpectedly young. Their detrital zircon ages continue via the Permian until the Late Triassic, Middle Jurassic and Early Cretaceous. The high-grade metamorphic rocks of the Asterousia crystalline complex are likely equiva

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Fernandez, Naiara, Magdalena Scheck‐Wenderoth, Mauro Cacace, and Ershad Gholamrezaie. "The Inherited Crustal Structure and Lithospheric Thermal Field Beneath the Sea of Marmara (NW Türkiye): Observations From 3D Gravity Modeling and Seismic Tomography Analysis." Journal of Geophysical Research: Solid Earth 129, no. 12 (2024). https://doi.org/10.1029/2024jb030336.

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AbstractThe North Anatolian Fault (NAF) extends for over 1,000 km across Türkiye and poses significant seismic hazard in the region. The Main Marmara Fault (MMF) segment of the NAF in the Sea of Marmara (NW Türkiye), exhibits along‐strike segmentation in its interseismic strain accumulation. Constraining the lithospheric configuration below the MMF is critical to understand its segmentation and assessing seismic hazard in the area. We present a new 3D lithospheric‐scale density of the Sea of Marmara, that combines gravity modeling and seismic tomography analysis. Using forward and inverse grav

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Kaygısız, Ersin, Namık Aysal, and Kıymet Deniz Yağcıoğlu. "Detrital zircon and rutile U–Pb dating of garnet-mica schist in the Istranca (Strandja) Massif (NW Türkiye): Mineral chemistry and metamorphic conditions." Geochemistry, August 2024, 126172. http://dx.doi.org/10.1016/j.chemer.2024.126172.

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Ekinci Şans, Bala, Şenel Özdamar, Fahri Esenli, and Stoyan Georgiev. "First U–Pb zircon and (U-Th)/He apatite ages of the Paleo-Tethys rocks in the Strandja Massif, NW Turkey: implications from newly identified serpentinite body." Arabian Journal of Geosciences 15, no. 14 (2022). http://dx.doi.org/10.1007/s12517-022-10562-z.

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Gumsley, Anna, Krzysztof Szopa, David Chew, et al. "An early cretaceous thermal event in the Sakar Unit (Strandja Zone, SE Bulgaria/NW Turkey) revealed based on U Pb rutile geochronology and Zr-in-rutile thermometry." Lithos, April 2023, 107186. http://dx.doi.org/10.1016/j.lithos.2023.107186.

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