Literatura científica selecionada sobre o tema "Le Grand Kurdistan"
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Artigos de revistas sobre o assunto "Le Grand Kurdistan":
Ünal, Mustafa Coşar, e Marina Miron. "Losing a war while defeating the enemy". Revista Científica General José María Córdova 20, n.º 40 (1 de outubro de 2022): 989–1023. http://dx.doi.org/10.21830/19006586.992.
Hajimam, Aveen, Hamdia Ahmed e Kathryne Mishkin. "Women's expectations of health care providers in the labor and delivery room in the Kurdistan Region of Iraq". Zanco Journal of Medical Sciences 27, n.º 1 (26 de abril de 2023): 42–52. http://dx.doi.org/10.15218/zjms.2023.007.
Ahmed, Hamdia Mirkhan, e Pola Farhad Hassan. "Assessment of hemorrhoids and anal fissure occurrences in women during pregnancy in Pirmam City/Iraq". Kufa Journal for Nursing Sciences 5, n.º 2 (13 de outubro de 2015): 349–55. http://dx.doi.org/10.36321/kjns.vi20152.2579.
Dhahir, Asmar, e Shahla Alalaf. "Maternal and neonatal characteristics that influence early neonatal deaths in a maternity teaching hospital". Zanco Journal of Medical Sciences 26, n.º 2 (14 de agosto de 2022): 96–107. http://dx.doi.org/10.15218/zjms.2022.011.
Bnar Sardar Yaseen Al-Sardari, Suzan Kh. Younus e Zainab Sardar Yaseen Al-Sardari. "Prevalence of anemia among pregnant women in their first antenatal care visit in Erbil City: A cross sectional study". Tikrit Journal of Pure Science 25, n.º 5 (18 de dezembro de 2020): 1–8. http://dx.doi.org/10.25130/tjps.v25i5.283.
Gunter, Michael. "Delisting the PKK as a Terrorist Organization". Commentaries 2, n.º 1 (1 de março de 2022): 25–38. http://dx.doi.org/10.33182/tc.v2i1.2122.
Aliyeva, A. I. "Turkey’s Assistance to Iraq after 2014: Key Determinants and Components". Moscow University Bulletin of World Politics 12, n.º 1 (19 de novembro de 2020): 121–49. http://dx.doi.org/10.48015/2076-7404-2020-12-1-121-149.
"The Pathway of the Opposition in the Kurdistan Region: Gorran as a Model". Journal for Political and Security Studies 2, n.º 3 (junho de 2019): 101–30. http://dx.doi.org/10.31271/10020.
Saeed, Nahwi. "The Past Explains the Present: Dealing with Anfal in the Kurdistan Region". Review of Middle East Studies, 27 de janeiro de 2023, 1–11. http://dx.doi.org/10.1017/rms.2022.21.
"Process of Grant and Promotion of Scientific Title in Academic Institutions of Kurdistan Region in the Light of Applicable Legislations". Qalaai Zanist Scientific Journal 4, n.º 2 (24 de março de 2019). http://dx.doi.org/10.25212/lfu.qzj.4.2.23.
Teses / dissertações sobre o assunto "Le Grand Kurdistan":
Braud, Jean. "La Suture du Zagros au niveau de Kermanshah (Kurdistan iranien) : reconstitution paléogéographique : évolution géodynamique, magmatique et structurale". Paris 11, 1987. http://www.theses.fr/1987PA112506.
The Zagros Range extends along the NE border of the Arabian plate for a distance of about 2 000 km, where it results from the convergence of the Arabian and Eurasiatic plates, the latter represented by Central Iran. Studies in the Kermanshah area (Iranian Kurdistan) reveals the presence of a suture zone between the two main blocks: an Outer Zagros or Folded Belt (area of oil production) forms the SW edge of the suture and constitutes the margin of the Arabian plate. The second block, the Zagros metamorphic domain or Sanandaj -Sirjan zone, constitutes the NE edge of the suture. Within the suture zone itself, strongly crushed units represent the remnants of oceanic crust formed during the Upper Triassic. Outliers of this domain are represented by ophiolites of the Sahneh-Harsin unit and radiolaritic of the Kermanshah unit formed during the Mesozoic within a narrow trough oriented parallel to the Arabian plate margin and separated from the oceanic crust by a continental barrier comprising carbonates (Bisitoun limestones). At the end of the Cretaceous, the NE drift of the Arabian plate induced a contraction of the domain and it’s partial over thrusting upon the margin of the Arabian plate (ophiolite obduction and Cretaceous nappes). However, during Eocene time,a narrow trough (Gaveh Rud domain) with oceanic basement remained (called the "Residual Tethys"). It was marked by magmatic activity and by flysch-type sediments. At the end of the Eocene this domain was again crushed and the Tethys Ocean disappeared permantly. Since the Oligo-Miocene the two continental blocks have been in perpetual collision with large continental thrusting associated with major lateral displacement along the Main Zagros Thrust, these movements causing modern seismic instability