As one of the most prominent and committed poets and writers of the Islamic Revolution, Seyed Hasan Hosseini, has paid attention to satire in three of his works. Through a descriptive-analytical method, the present study is dedicated to analyze the types, the techniques and the themes of satire have been used in these works: "Boradeh-ha"(the swarfs), "Nooshdarouye Tarhe Generic" (The panacea of generic plot) and "Festivale Khanjar" (the Dagger Festival). Hosseini has used, in above-mentioned works, aphorism, classic poetry format, Nimaei (Nimaic) poetry and white (Shamloi) poetry. Regarding that satirical tales are generally classified into three categories of "dramatic", "narrative" and "poetic", it can also be claimed that the satires used in these works are mostly dramatic using the techniques of exaggeration and sarcasm, especially poetic satires using the techniques of simile and metaphor. In addition, the most frequent theme of his satires has been the cultural critiques in the field of art as well as social critiques in the field of economy.

The Khanjar Pb- Ag (Zn) deposit is one of the stratabound deposits of Cretaceous age in Central Iran. The ore bodies may be grouped into two main geometric types: I) Lenses of ore bodies congruent with bedding, 2) Ores as open space filling or with brecciate fabric due to faulting. Both types occur in limestone unit (k2b).Three ore bearing facies have been distinguished in the Khan jar area: I) Siliceous limestone facies; galena, sphalerite and pyrite are the main ore minerals.Minor amounts of chalcopyrite are also visible. 2) Mullusca, Echinoderm wackstone facies with galena and sphalerite. 3) Rudist limestone facies with large amount of galena. As with other stratabound and stratiform Pb- Zn deposits, the main ore minerals are simple and few in number. In addition, galena, sphalerite and pyrite, some tetrahedrite, barite and minor amounts of copper minerals are observed. Pyrite often with rframboidal texture and sphalerite with spheroidal texture form always part of paragenesis. Fluid inclusion investigations on saddle dolomite located in fractures with galena and sphalerite demonstrated the homogenization temperature of 145-230 centigrade and salinity of 17.5-23% NaCl equivalent. Geometry of ore bodies, occurrence of ore horizons in certain sedimentary facies, ore textures and structures, depositional environment (Lagoonal), paragenetic sequence of minerals and fluid inclusion data, all suggest that Khanjar Pb- Ag (Zn) deposit is an MVT deposit.

Torkmans are a branch of the Middle Asian Turks that had a nomadic life in the extended deserts of the lower region of the Seyhoon River and the Aral River from the ancient age. After the Collapse of Goog Turk Empire a group of turks that were calld Aghooz, separated of them and immigrated from Archon region to Aral and Sayir Sea. The main centers of settlement of Turkmens are: Turkmenistan, Iran, Afghanistan, Iraq, Turkey, Jordan, Syria, China, Tajikistan, Russia, and Uzbekistan. Iran is one of the main settlements of Turkmens. Iranian Turkmens live in eastern south of Caspian Sea and Turkmen Sahra. They have scattered in the Provinces of Golestan, Razavi Khorasan and North Khorasan. Their population is about 2 million people. Turkmen, Aghghola and Gonbad Ghaboos are the important cities of Turkmens in Iran. From the eleventh century, first the name of Turkmen was used as a plural name of "Turkmanan" by Iranian authors such as Gardizi and Beyhaghi then it was used in the same meaning "Aghoz" in Turky and Ghoz in Arabic and Persian. In the first of eightieth, the term of "Oghoz" was used for the first time in Turkish language on the Copings in Mongolia. Oghozes was a major part of nomadic Empire that was extended from China to border provinces of Iran, Bizans and Volga River. According of these copings, Oghozes were formed of nine tribes. Some of authors believe that Oghozes were 24 tribes. For the first time, the name of Turkmen was raised in the last of tenth century. Study on the origin and meaning of the word of Turkmen shows that Non-Muslim Oghozes called Muslim Oghozes "Turkmen". Later, the name of Turkmen was used by Oghozes. Although they didn't forgot their ancestral name but events of the second half of the tenth century and the first half of the eleventh century played an important role in the Oghorian history. These events included of the conversion to Islam and The emergence of the government of Seljuqi. In this time, Oghozes didn't have a "Khan" but they had a Yabgho (king).

Ferdowsi was an outstanding orator, a messenger of freedom, not one with a sense and spirit to please the rulers of the time, nor a poet laureate composing his poems upon orders of rulers', neither affiliated to any court. This national poet was the creator of the central and basic locus of stories, as well as the founder of national palace of poetic language and philosophic rhetoric. What makes Ferdowsi outstanding among other poets is his role in dissemination of vitalizing the beam of nationalism within the frameworks of conventional principles and hereditary traditions. Indeed, The Shahnameh is a masterpiece, whose poet has elegantly mixed many sayings with various profound subjects such as method of statesmanship, military organization, freedom, nobility, love of Iran, knowledge of Iran, philosophic and mystic ideas, profound and wonderful thoughts, and ways for living. To know more about the culture, knowledge, overflowing sources of thought and feeling, and mental interests of Iranian people, one must know the Shahnameh and study it deeply. In this article, we are going to discuss the relations between Iran and India, based on a new research on Indian words that the great Ferdosi has used in his grand epic.

Introduction: Forugh Farrokhzad (1935–1967) and Ahmad Shamlou (1925–2000) are two prominent poets of the She’r-e Nou (New Poetry) Nimaic movement, whose works are overshadowed by nihilism. In their inclination toward nihilism, the component of love is directly connected, such that love—in both individual and social dimensions—has influenced their nihilistic tendencies. This article examines the nature of this influence and the perspectives of the two poets.   Research Method The statistical population of this research comprises the collected poems of Farrokhzad and Shamlou. Through library research, data on the relationship between love and their nihilistic thoughts were extracted via note-taking. By categorizing the content of these notes, the article was written using a descriptive-analytical method.   Discussion Nihilism derives from the word nihil (meaning "nothing" or "void") (Shayegan, 1999: 13). Terminologically, it translates to "nothingness-ism" or "negationism" (Zaršanās, 2006: 13). Various dimensions of nihilism appear in the poetry of Farrokhzad and Shamlou, with the influence of the love component evident in the following aspects:   The Love Component in Political Nihilism Political nihilism expanded in contemporary literature during the She’r-e Nou movement following the 1953 coup d’état. Part of Shamlou’s poetic nihilism is political. However, Farrokhzad did not engage with politics during that period. The themes of absurdity in Shamlou’s poems from this era are linked to romantic despair toward the struggling human, as seen in the poem "Sorud-e Mardi ke Tanhā Mi-ravad" (Anthem of the Man Walking Alone), where the description of "Khanjar az posht khordan" (being stabbed in the back) expresses ultimate despair.   The Love Component in Social Nihilism Social nihilism in Farrokhzad and Shamlou’s poetry relates to their view of love in society. Their nihilistic thoughts converge on the absence of love in society, yet each reflects from their own perspective. Farrokhzad (early period) despairs societal attitudes in a patriarchal society. Her nihilism also stems from personal struggles and marital failure, generalized to society. Shamlou’s social nihilism connects love’s decay to societal decline and the lack of affection among people, influenced by political conditions.   The Love Component in Individual Nihilism This dimension is more prominent in Farrokhzad’s poetry than Shamlou’s. Emotional failure cast nihilism over her work, which she never transcended. Her most bitter experience—marriage and divorce—fueled nihilistic thought in her poetry. Her primary reason for nihilism is the absence of a sublime beloved, leading to persistent death imagery, as in: "The savior sleeps in the grave / and the earth, the accepting soil / is a gesture toward tranquility" (Farrokhzad, 2005: 298). Shamlou’s romantic nihilism emerged in the 1950s. After the coup, he was imprisoned, post-release, his first wife divorced him. A second marriage also failed. This defeat—compounded by socio-political disillusionment and societal decay—drove him to romantic nihilism, pushing him to the brink of suicide. This is reflected in poems like "Ghazal-e Bozorg" (Grand Ghazal), where love is likened to "an empty birdcage. " However, Shamlou transcended this nihilism through sublime love with Āydā.   Conclusion Results indicate that the link between love and individual nihilism is frequent in both poets’ works but also extends to political-social nihilism. Both poets’ emotions are intrinsically tied to the love component. The decay of love among people, absence of love in life, and romantic failures drive their nihilistic tendencies.

Introduction The NE-trending Torud-Chahshirin metallogenic belt, lying in the central to the eastern portion of the Alborz Mountain system is approximately 300 km in length, with a complex tectonic, magmatic, and stratigraphic history (Alavi, 1996). The major ore deposits of the Torud-Chahshirin metallogenic belt (Fig. 6) include many mineral occurrences and abandoned mines, particularly epithermal precious and base metal veins, hosted by volcanic and subvolcanic alkaline rocks, such as Gandy, Abolhassani, Cheshmeh Hafez, Ghole Kaftaran, Pousideh, Darestan and Chahmessi (Shamanian et al, 2004,Fard et al, 2006,Mehrabi and Ghasemi, 2012). In addition, other types of deposit in the district include turquoise and placer gold at Baghu (Au ± Cu), Fe–skarn deposits at Chalu, and Pb–Zn (Ag) carbonate-hosted deposits (MVT) at Reshm, Khanjar and Anarou (Shamanian et al, 2004,Niroomand et al, 2018). The Northern Chah-Farsakh deposit is located 75 km south of Damghan city, and lies within the western part of the Torud-Chahshirin metallogenic belt. This paper describes the local stratigraphic and geological features together with, the relationships between the copper mineralization and the host rocks. Descriptions are supplemented by fluid inclusion studies to constrain the conditions for the genesis of the Northern Chah-Farsakh deposit. Materials and methods This study focused on the geological and mineralogical of the Northern Chah-Farsakh deposit. Determination of the mineralogy and paragenesis of the deposit is based on logging of drill cores and petrographic studies of over 48 polished thin and thick sections, supplemented by XL30 scanning electron microscopy conducted at Tarbiat Modares University. Doubly polished wafers using standard techniques were prepared from seven samples collected in the presumed feeder zone of the Northern Chah-Farsakh deposit. Micro-thermometric measurements of fluid inclusions were performed on a Linkam THMS 600 combined heating/ freezing stage with a German Zeiss microscope at the Tarbiat Modares University, Iran. Results and discussion The Northern Chah-Farsakh copper deposit is located in the Torud-Chahshirin metallogenic belt and formed in the Neoproterozoic-early Cambrian volcanic-sedimentary sequence. Mineralization occurred in the form of a sulfide horizon in the meta-volcanic rocks. It formed less frequently in the hanging wall units of meta-volcanic, including the muscovite-quartz schist, the meta-sandstone, the tuffaceous sandstone, and the marble units. The main ore minerals in the deposit include chalcopyrite, pyrite, sphalerite magnetite, pyrrhotite, tetrahedrite, tennantite and bornite, respectively, and the secondary minerals include covellite and chalcocite, and the most abundant gangue minerals are quartz and calcite. Based on the orebody structure, mineralogy, and ore textures, we recognize tree different ore facies types in the Northern Chah-Farsakh deposit: 1) stockwork/feeder zone,2) massive ore facies,and 3) bedded ore facie. Siliceous and carbonate alterations are the main alterations associated with mineralization. Banded, disseminated, replacement, massive, veins-veinlets are main ore-bearing textures in this deposit According to fluids inclusion studies on the quartz minerals of the stringer zone, the average homogenization temperature of the fluids inclusions is 355 °C and the salinity is 6 to 16 wt% NaCl eq. Conclusion According to geological studies, mineralogy, structure and texture and fluids inclusions the Northern Chah-Farsakh deposit is formed in the submarine volcanic activity environment and this deposit shows most similarities with the Besshi-type VMS mineralization.