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[The Zeda Ranch, west of Puebla.]
No full textRecto: [imprinted on negative] El Zeda Poniente del Rancho de Mi Puebla. Fot. - J. Rodriguez Avalos - Puebl
descrizione degli apparecchi - guida pratica per la posa in opera
No full textScheda di catalogo BiblioUniTS Suonerie telefoni parafulmini : descrizione degli apparecchi : guida pratica per la posa in opera / Umberto Zeda. - Milano : Biblioteca di elettricità, 1904. - 183 p. : ill. ; 20 cm Percorso narrativo - smaTs </center
Para la salcedocoronelización de la Fábula de Equis y Zeda
Full text linkFábula de Equis y Zeda has been considered text of irrational construction and therefore of difficult or impossible comment. Starting from three keys of Gerardo Diego (cubist or creationist militancy, dedication to the study of gongoristic and after-gongoristic poetry, and recovery of the genre of mythological fable), Equis y Zeda is revealed here as poem whose argument depends on intertextuality of a certain composition that Gabriel Bocángel published in La lira de las musas (1637
MINDIETI COMMUNITY (ZEDA MACHAKHELI, REPUBLIC OF TURKEY)
Full text linkhttps://geohistory.humanities.tsu.ge/ge/procedings/83-shromebi/147-shromebi-6.htmlMindieti community (“Maral”) is in Zeda (Upper) Machakheli. Zeda (Upper) Machakheli belongs to Turkey from 1921 while Kveda (Lower) Machakheli was a part of Georgia occupied by Bolshevik Russia. Machakheli gorge was declared a closed zone by the Soviet Union as well as by the Republic of Turkey; the communication between the two parts of gorges was forbidden for sixty years. After creation of the Republic of Georgia the relations between the relatives living in different parts of the gorge have been restored. Zeda (Upper) Machakheli (Jamili in Turkish) consists of 6 communities: Khertvisi, Zedvake, Eprati, Kvabitavi, Mindieti, Akria. There are several villages (Mahalea) in every community. The administrative centre of Zeda (Upper) Machakheli is Khertvisi, Borchkha district, vilayet (region) of Artvin. Nowadays there are 500 families in Zeda (Upper) Machakheli, almost half of them stay in gorge for winter. It is pleasant that after the retirement people from Machakheli return to their motherland from big cities. Mindieti community is situated in Didghele gorge. There are some other streams in Mindieti: Tsivnareti stream, Zekaleti Stream etc. Zeda (Upper) Machakheli is recognized to be a protected territory by UNESCO. There are several big and small villages in Mindieti community: Iremeti, Zekaleti, Osaneti, Kavtareti, Givieti, Tsetskhleti, Konkalati, Zemtkisi, Zemvare (Givieti’s Sakaria, Mahale), the half of Veli, the half of Tsiakhi, Tsivnareti, Kortaneti, Gogortke, Jorieti, Didtke. The population of Mindieti is ethnically Georgian. The old name of Machakheli is Michikhiani. Michikhiani was a part of eparchy of Tbeti. From 1878 Machakheli was under the jurisdiction of the Russian Empire. As a result of the Russian anti-Georgian policy, many Georgians left the gorge in 1881-1882 as well as in 1921. The memory about Georgian surnames is saved in Mindieti. There are several surnames which are represented in an unchanged form, for example Iremadze, Katamadze, Tsivnaridze, Giviadze etc. A large part of surnames have Islamic form: Ikhtiaroghli, Metinoghli etc. After creation of the Republic of Turkey new Turkish surnames were given to the population of Mindieti as well as to the citizens of Turkey. The knowledge about the traditional agricultural-economic relations between historical Georgian regions – Zeda (Upper) Machakheli, Nigali/Ligani, Shavsheti (the Republic of Turkey nowadays) and Adjara is saved in population. Unlike other parts of historical Georgia, the migration processes are not common in Zeda (Upper) Machakheli. The number of population in Mindieti community decreases in winter, but several families stay in almost every village. The type of settlement in Zeda (Upper) Machakheli is traditionally Georgian, Khevispiruli. Villages and dwellings are situated in vertical zone. Villages are divided into districts. The people with the same surnames, close relatives live mainly in districts. The dwellings in Zeda (Upper) Machakheli are traditionally made of chestnut trees, with the stone foundations, covered with lath distilled from spruce or tiles; they represent the local varieties of Adjarian house. The indivisible parts of the dwellings are barn and granary. From the traditional branches of economy they still follow agriculture (wheat is almost wholly replaced by maize) and stock farming (they have cattle, goats, sheep). Growing maize is the main branch of economy in Machakheli. A big part of cornfields and mowing lands has been covered with hazelnut bushes during the past twenty years, because they are important sources of income. The traditional Georgian mutual aid form – Nadi is saved as well as some kind of vine varieties (Chkhaveri). The vine grows up on the high trees, mainly on the Leki (maple) tree. People in Mindieti have gardens. The traditional food system in Zeda (Upper) Machakheli mainly consists of dairy products and vegetables. The traditional forms of stock farming coexist with the modern life. Every village has its own Mta (Mereta). The folk feast of Shuamtoba was held traditionally in the mountains. The subsidiary branch of the economy – bee-keeping is also developed. From the traditional branches of handicraft wood carpenter and partly blacksmith’s work is preserved. The tradition of weaving is saved in elderly women. The looms are kept in families.
The traditional family and economic equipment and the rules of their production is preserved in Mindieti as well as the wooden covered bridge of rare construction and beauty and comparatively new stone arched bridge, which is built according to the traditional Georgian architectural standards. The older generation remembers some elements of traditional spiritual culture, for example, New Year; the fragments of folk feast of Garegnoba (Gargnoba) are preserved as well as the legends about King Tamar. There are several Jameh mosques. The oldest is the Mindieti Jameh; the elements of the traditional Georgian ornaments can be seen in its internal carvings. Zeda (Upper) Machakheli is also interesting linguistically. Among Georgian historical-ethnographic regions, which are the part of Turkey, only Machakheli has no threat of losing the Georgian language at this stage
Entre el Barroco y la Vanguardia. La "Fábula de Equis y Zeda" de Gerardo Diego
No full textRESUMEN En el presente artículo se analiza la Fábula de Equis y Zeda, destacando cómo esta obra se sustenta sobre la unión de principios o elementos opuestos: desde el propio molde paródico empleado (imagen creacionista frente a retórica clásica) al régimen diurno de la imagen (que concede homogeneidad a la libertad extrema de la metáfora pero entraña asimismo una concepción polémica de la realidad). La anécdota amorosa conforma igualmente una composición metaliteraria en torno al poeta vanguardista, si bien desde una estética humorística (“barroco de la levedad”) que pretende recrear la realidad como maravilla y sorpresa continuas. ABSTRACTIn the present article we analyse the "Fábula de Equis y Zeda", emphasizing how this work is based on the union of opposed principles or elements: from the proper parodic pattern used (creationist image opposed to classical rhetoric) to “day image regime” (that supplies homogeneity to the extreme freedom of metaphor but implies at the same time a polemical conception of reality). The love anecdote forms a metaliterary composition around the avant-garde poet but from a humorous esthetic (“baroque of lightness”) that tries to recreate reality as continuous marvel and surprise.
Going Beyond Counting First Authors in Author Co-citation Analysis
Full text linkThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
New evidence for supra-subductionzone ophiolites in the Vardar Zone from the Vermion Massif (northern Greece): Implication for the tectono-magmatic evolution of the Vardar oceanic basin
No full textThe Vermion Massif (northern Greece) is located across the boundary between the Pelagonian and Vardar Zones and includes several tectonic units bearing ophiolitic rocks, which represent remnants of the oceanic lithosphere formed in the Neotethyan Vardar Ocean, between the Pelagonian and the Serbo-Macedonian continental realms. This massif consists of tectonic units belonging to the Pelagonian Domain, which are tectonically overlain by units associated with the Almopias sub-Zone (Vardar Zone). Ophiolitic rocks consist of mantle harzburgites and ophiolitic mélanges. The ophiolitic mélanges incorporate rocks exhibiting a wide range of composition, including various intrusive rocks and volcanic rocks ranging from basalts, basaltic andesites, andesites, dacites, to rhyolites. Incompatible elements and rare earth elements analyses indicate that a number of different rock-types formed in distinct tectonic settings can be identified. Mantle harzburgites have a very depleted nature and represent portions of the supra-subduction (SSZ) mantle developed in an intra-oceanic arc setting. The mélanges units include six rock types variably distributed in the Pelagonian and Almopias Units. They are: (1) calc-alkaline rocks with marked depletion in Nb, Ta Ti and enrichment in LREE, Th; (2) LREE-depleted N-MORB; (3) LREE-enriched E-MORB; (4) alkaline within-plate basalts showing marked enrichments in Th, Ta, Nb, LREE; (5) low-Ti island arc tholeiites featuring depletion in HFSE; and (6) very-low-Ti boninites characterized by strong depletion in HSFE and REE. Previous interpretations have referred the Vardar ophiolites to a MORB-type oceanic setting and to a MORB-type backarc setting; however, the widespread occurrence of SSZ ophiolites has never been documented in the Vardar Zone before and is particularly important as it testifies for the existence of an intra-oceanic arc basin in the Vardar oceanic domain. The results presented in this paper compared with literature data on other magmatic rocks within the Vardar Zone suggest that the opening and closure of the Vardar Ocean record several distinct accretion events in this basin, that is oceanic crust generation at mid-ocean ridge, alkaline seamounts in the oceanic domain and SSZ setting, as well as two accretion events in the western realm of the Serbo-Macedonian continent, that is volcanic arc and backarc settings. Based on the comparison between the modern west Pacific subduction system and the results from this study a new model for a multistage tectono-magmatic evolution of the Vardar Ocean is proposed
New evidence for supra-subduction zone ophiolites in the Vardar zone of Northern Greece: implications for the tectono-magmatic evolution of Vardar Oceanic Basin.
No full textThe Vermion Massif (northern Greece) is located across the boundary between the Pelagonian and Vardar Zones and includes several tectonic units bearing ophiolitic rocks, which represent remnants of the oceanic lithosphere formed in the Neotethyan Vardar Ocean, between the Pelagonian and the Serbo-Macedonian continental realms. This massif consists of tectonic units belonging to the Pelagonian Domain, which are tectonically overlain by units associated with the Almopias sub-Zone (Vardar Zone). Ophiolitic rocks consist of mantle harzburgites and ophiolitic mélanges. The ophiolitic mélanges incorporate rocks exhibiting a wide range of composition, including various intrusive rocks and volcanic rocks ranging from basalts, basaltic andesites, andesites, dacites, to rhyolites. Incompatible elements and rare earth elements analyses indicate that a number of different rock-types formed in distinct tectonic settings can be identified. Mantle harzburgites have a very depleted nature and represent portions of the supra-subduction (SSZ) mantle developed in an intra-oceanic arc setting. The mélanges units include six rock types variably distributed in the Pelagonian and Almopias Units. They are: (1) calc-alkaline rocks with marked depletion in Nb, Ta Ti and enrichment in LREE, Th; (2) LREE-depleted N-MORB; (3) LREE-enriched E-MORB; (4) alkaline within-plate basalts showing marked enrichments in Th, Ta, Nb, LREE; (5) low-Ti island arc tholeiites featuring depletion in HFSE; and (6) very-low-Ti boninites characterized by strong depletion in HSFE and REE. Previous interpretations have referred the Vardar ophiolites to a MORB-type oceanic setting and to a MORB-type backarc setting; however, the widespread occurrence of SSZ ophiolites has never been documented in the Vardar Zone before and is particularly important as it testifies for the existence of an intra-oceanic arc basin in the Vardar oceanic domain. The results presented in this paper compared with literature data on other magmatic rocks within the Vardar Zone suggest that the opening and closure of the Vardar Ocean record several distinct accretion events in this basin, that is oceanic crust generation at mid-ocean ridge, alkaline seamounts in the oceanic domain and SSZ setting, as well as two accretion events in the western realm of the Serbo-Macedonian continent, that is volcanic arc and backarc settings. Based on the comparison between the modern west Pacific subduction system and the results from this study a new model for a multistage tectono-magmatic evolution of the Vardar Ocean is proposed
Variations on the Author
Full text link“Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship
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