Mysticism in the poetry of Emily Dickinson: a theological interpretation

This paper is an attempt to analyze the poetry of Miss Emily Dickinson (1830-1886) in order to reveal the extent of mysticism in it, and it focuses on the concept of “theology.” Mysticism involves a deep, almost obsessive, concern with such problems as death, the existence of the soul, immortality, the existence of God and heaven, salvation or redemption, etc. The critical approach was used to analyze some of Dickinson’s major poems. A glance at her poetry reveals that it shows an extreme preoccupation with the effect of death and explores various themes such as the nature of the soul, the problem of immortality, the possibility of faith and the reality of God. The researchers also tried to reveal the internal and external influences that shaped Dickinson’s poetry. The paper concluded that the theme of death was inexhaustible for her. If her poetry seldom became “lyrical,” seldom departed from the colorless sobriety of its bare iambics and toneless assonance, it did so most of all when the subject was death. Although Dickinson’s poetry contains some mystical elements, mystical poetry, in the traditional sense, at least, is not her special poetic gift

Geoquímica del rango volcánico alcalino del eoceno medio-superior, parte sur de las montañas centrales de Alborz, norte de Irán

The Ziaran volcanic Belt (ZVB), North of Iran contains a number of intra-continental alkaline volcanic range situated on South part of central Alborz Mountains, formed along the localized extensional basins developed in relation with the compressional regime of Eocene. The mid-upper Eocene volcanic suite comprises the extracted melt products of adiabatic decompression melting of the mantle that are represented by small volume intra-continental plate volcanic rocks of alkaline volcanism and their evaluated Rocks with compositions representative of mantle-derived, primary (or near-primary) melts. Trace element patterns with significant enrichment in LILE, HFSE and REEs, relative to Primitive Mantle. Chondrite-normalized of rare earth elements and enrichment in incompatible elements and their element ratios (e. g. LREE/HREE, MREE/HREE, LREE/MREE) shown these element modelling indicates that the magmas were generated by comparably variable degrees of partial melting of garnet lherzolite and a heterogeneous asthenospheric, OIB mantle sources.El cinturón volcánico de Ziaran (ZVB), al norte de Irán, contiene una serie de cordilleras volcánicas alcalinas intracontinentales situadas en la parte sur de las montañas centrales de Alborz, formadas a lo largo de las cuencas extensionales localizadas desarrolladas en relación con el régimen de compresión del Eoceno. La suite volcánica del Eoceno medio superior comprende los productos de fusión extraídos de la fusión por descompresión adiabática del manto que están representados por rocas volcánicas de placa intracontinental de pequeño volumen de vulcanismo alcalino y sus rocas evaluadas con composiciones representativas de las rocas derivadas del manto, primarias (o cercanas). -primaria) se derrite. Patrones de oligoelementos con enriquecimiento significativo en LILE, HFSE y REE, en relación con Primitive Mantle. Condrita normalizada de elementos de tierras raras y enriquecimiento en elementos incompatibles y sus proporciones de elementos (por ejemplo, LREE / HREE, MREE / HREE, LREE / MREE) que muestra el modelado de estos elementos indica que los magmas se generaron por grados comparativamente variables de fusión parcial de granate lherzolita y fuentes de manto OIB astenosféricas heterogéneas

Geoquímica del rango volcánico alcalino del eoceno medio-superior, parte sur de las montañas centrales de Alborz, norte de Irán

The Ziaran volcanic Belt (ZVB), North of Iran contains a number of intra-continental alkaline volcanic range situated on South part of central Alborz Mountains, formed along the localized extensional basins developed in relation with the compressional regime of Eocene. The mid-upper Eocene volcanic suite comprises the extracted melt products of adiabatic decompression melting of the mantle that are represented by small volume intra-continental plate volcanic rocks of alkaline volcanism and their evaluated Rocks with compositions representative of mantle-derived, primary (or near-primary) melts. Trace element patterns with significant enrichment in LILE, HFSE and REEs, relative to Primitive Mantle. Chondrite-normalized of rare earth elements and enrichment in incompatible elements and their element ratios (e. g. LREE/HREE, MREE/HREE, LREE/MREE) shown these element modelling indicates that the magmas were generated by comparably variable degrees of partial melting of garnet lherzolite and a heterogeneous asthenospheric, OIB mantle sources.El cinturón volcánico de Ziaran (ZVB), al norte de Irán, contiene una serie de cordilleras volcánicas alcalinas intracontinentales situadas en la parte sur de las montañas centrales de Alborz, formadas a lo largo de las cuencas extensionales localizadas desarrolladas en relación con el régimen de compresión del Eoceno. La suite volcánica del Eoceno medio superior comprende los productos de fusión extraídos de la fusión por descompresión adiabática del manto que están representados por rocas volcánicas de placa intracontinental de pequeño volumen de vulcanismo alcalino y sus rocas evaluadas con composiciones representativas de las rocas derivadas del manto, primarias (o cercanas). -primaria) se derrite. Patrones de oligoelementos con enriquecimiento significativo en LILE, HFSE y REE, en relación con Primitive Mantle. Condrita normalizada de elementos de tierras raras y enriquecimiento en elementos incompatibles y sus proporciones de elementos (por ejemplo, LREE / HREE, MREE / HREE, LREE / MREE) que muestra el modelado de estos elementos indica que los magmas se generaron por grados comparativamente variables de fusión parcial de granate lherzolita y fuentes de manto OIB astenosféricas heterogéneas

MINERAL CHEMISTRY AND GEOCHEMISTRY OF GRANITOID ROCKS IN NORTHERN OF SARDUIEH (DASHT SHAGHIN AND SARTASHTAK), IRAN

Dehaj-Sarduieh volcano-plutonic belt in Kerman province of Iran represents a part of Urumieh-Dokhtar Magmatic assemblage which is mainly composed of granodiorite, quartz diorite, tonalite granite and granophyre. These rocks emplaced in Eocene volcanic and pyroclastic deposits rocks and are considered to be Oligo-Miocene in age. Geochemical studies showed that the amphibole minerals in diorite and granodiorites are calcic in composition and range from actinolite to magnesio-hornblende. Geochemical and mineralogical results revealed that these bodies have been generated in the lower part of the lower crust at a temperature of 700 to 750 °C, with an oxygen fugacity of -13.57 to -15.76 and a low pressure of 1 to 3 kb through mixing of mantle-derived mafic magma with crustal-derived felsic melts. These amphiboles are subduction-related and in accordance with the tectono-magmatic features suggested for these massifs, they show the characteristics of subduction and active continental margin environments. Field observations and mineralogical-geochemical evidence revealed that the original magma has been calc-alkaline in composition and metaluminous I-type. It is also showed that the process of fractional crystallization has significantly contributed in the formation of these rocks. Sarduieh igneous rocks displayed an enrichment in the large-ion lithophile elements (LILE, e.g. Ce, Th, Ba, Zr, Sr) and a depletion of the high field strength elements (HFSE, e.g. Nb, P, and Ti) and Chondrite normalized REE patterns are characterized by LREE enrichment and Show slight negative Eu anomalies which reflect the influence of subductions zone and active continental margin environments. The tectonic setting of these rocks is inferred to be continental arc or active continental margin and they were deduced to be generated by the subduction of the Neotethys oceanic crust beneath the Central Iranian continental plate.O cinturão vulcânico-plutônico de Dehaj-Sarduieh, na província de Kerman, no Irã, representa uma parte do conjunto Urumieh-Dokhtar Magmatic, composto principalmente de granodiorito, diorito de quartzo, granito e granito. Essas rochas localizadas em depósitos vulcânicos e piroclásticos do Eoceno e são consideradas como idade do Oligo-Mioceno. Estudos geoquímicos mostraram que os minerais anfibólio nos dioritos e granodioritos são de composição cálica e variam de actinolita a magnésio-hornblenda.Resultados geoquímicos e mineralógicos revelaram que esses corpos foram gerados na parte inferior da crosta inferior a uma temperatura de 700 a 750 ° C, com uma fugacidade de oxigênio de -13,57 a -15,76 e baixa pressão de 1 a 3 kb através da mistura de magma máfico derivado do manto com derretidos félsicos derivados da crosta. Esses anfibólios estão relacionados à subducção e, de acordo com as características tectono-magmáticas sugeridas para esses maciços, mostram as características dos ambientes de subducção e margem continental ativa. As observações de campo e as evidências mineralógico-geoquímicas revelaram que o magma original tem composição alcalino-calcária e tipo I metaluminoso. Também é mostrado que o processo de cristalização fracionada contribuiu significativamente na formação dessas rochas. As rochas ígneas de Sarduieh exibiram um enriquecimento nos elementos litófilos de íons grandes (LILE, por exemplo, Ce, Th, Ba, Zr, Sr) e um esgotamento dos elementos de alta força de campo (HFSE, por exemplo, Nb, P e Ti) e Condrita normalizados Os padrões REE são caracterizados pelo enriquecimento LREE e Mostrar pequenas anomalias negativas da Eu que refletem a influência da zona de subducção e ambientes ativos de margens continentais. O cenário tectônico dessas rochas é inferido como arco continental ou margem continental ativa e elas foram deduzidas para serem geradas pela subducção da crosta oceânica de Neotethys sob a placa continental iraniana central

Geoquímica del rango volcánico alcalino del eoceno medio-superior, parte sur de las montañas centrales de Alborz, norte de Irán

El cinturón volcánico de Ziaran (ZVB), al norte de Irán, contiene una serie de cordilleras volcánicas alcalinas intracontinentales situadas en la parte sur de las montañas centrales de Alborz, formadas a lo largo de las cuencas extensionales localizadas desarrolladas en relación con el régimen de compresión del Eoceno. La suite volcánica del Eoceno medio superior comprende los productos de fusión extraídos de la fusión por descompresión adiabática del manto que están representados por rocas volcánicas de placa intracontinental de pequeño volumen de vulcanismo alcalino y sus rocas evaluadas con composiciones representativas de las rocas derivadas del manto, primarias (o cercanas). -primaria) se derrite. Patrones de oligoelementos con enriquecimiento significativo en LILE, HFSE y REE, en relación con Primitive Mantle. Condrita normalizada de elementos de tierras raras y enriquecimiento en elementos incompatibles y sus proporciones de elementos (por ejemplo, LREE / HREE, MREE / HREE, LREE / MREE) que muestra el modelado de estos elementos indica que los magmas se generaron por grados comparativamente variables de fusión parcial de granate lherzolita y fuentes de manto OIB astenosféricas heterogéneas

The Petrology of Ziyran Volcanic Belt (ZVB) Eocene Volcanic Rocks

The Ziyaran Volcanic Belt (ZVB) is located in the southern part of central Alborz and in the Ziyaran area. The geology of this layer includes various kinds of stone units. In the north, they are the reminder of Cenozoic, quaternary deposits, and in the western part, the exposure stone units are mostly Precambrian and Paleozoic deposits and in the south-eastern part of the studied area, the stones belong to the Mesozoic era and specifically, the sediments belong to the Jurassic era are exposed. Also, the basic volcanic rocks that belong to the Eocene period are located in the Ziyaran area, in the western part of Taleqan County and in the Alborz state. This study aimed to evaluate the petrology of Ziyaran Volcanic Belt (ZVB) Eocene volcanic rocks. For this purpose, which is mostly focused on the study of Cretaceous stones in the central Alborz zone, sampling of the stones in the intended area was performed with the survey and field methods and for 120 samples. After the preparation of the thin layer from the well and without alteration samples, they were examined with petrography and petrology tests. The results of the petrology studies of the volcanic rocks of the Ziyaran area expressed that the basic volcanic rocks in the intermediate area with the intermediate- upper chemical composition of Eocene Alkaline Phosphatase (ALP) located in the central zone of Alborz heights, with lithology composition of Alkali olivine basalts and Andesite

The Petrology of Ziyran Volcanic Belt (ZVB) Eocene Volcanic Rocks

The Ziyaran Volcanic Belt (ZVB) is located in the southern part of central Alborz and in the Ziyaran area. The geology of this layer includes various kinds of stone units. In the north, they are the reminder of Cenozoic, quaternary deposits, and in the western part, the exposure stone units are mostly Precambrian and Paleozoic deposits and in the south-eastern part of the studied area, the stones belong to the Mesozoic era and specifically, the sediments belong to the Jurassic era are exposed. Also, the basic volcanic rocks that belong to the Eocene period are located in the Ziyaran area, in the western part of Taleqan County and in the Alborz state. This study aimed to evaluate the petrology of Ziyaran Volcanic Belt (ZVB) Eocene volcanic rocks. For this purpose, which is mostly focused on the study of Cretaceous stones in the central Alborz zone, sampling of the stones in the intended area was performed with the survey and field methods and for 120 samples. After the preparation of the thin layer from the well and without alteration samples, they were examined with petrography and petrology tests. The results of the petrology studies of the volcanic rocks of the Ziyaran area expressed that the basic volcanic rocks in the intermediate area with the intermediate- upper chemical composition of Eocene Alkaline Phosphatase (ALP) located in the central zone of Alborz heights, with lithology composition of Alkali olivine basalts and Andesite

The Role of Supply Chain Strategy and Affiliate Marketing in Increasing the Demand for E-Commerce – Social Media POV

Abstract- The study examined the most influential affiliate marketing and supply chain strategies that are most beneficial and usable through social media websites which can increase the demand on e-commerce. Through employing the quantitative approach; the researchers distributed total of (95) questionnaires on marketing managers within cosmetics companies in Jordan- Amman during the fiscal year (2018-2019). Results of study indicated a high level of awareness and dependency of cosmetics companies on marketing through social media websites as a form of endorsement. In addition to that, it appeared that among the chosen affiliate marketing strategies CPC/PPC was the most influential and usable strategy through social media as a form of endorsement and marketin

Targeting cancer signaling pathways by natural products: Exploring promising anti-cancer agents

Cancer is one of the leading causes of death and significantly burdens the healthcare system. Due to its prevalence, there is undoubtedly an unmet need to discover novel anticancer drugs. The use of natural products as anticancer agents is an acceptable therapeutic approach due to accessibility, applicability, and reduced cytotoxicity. Natural products have been an incomparable source of anticancer drugs in the modern era of drug discovery. Along with their derivatives and analogs, natural products play a major role in cancer treatment by modulating the cancer microenvironment and different signaling pathways. These compounds are effective against several signaling pathways, mainly cell death pathways (apoptosis and autophagy) and embryonic developmental pathways (Notch pathway, Wnt pathway, and Hedgehog pathway). The historical record of natural products is strong, but there is a need to investigate the current role of natural products in the discovery and development of cancer drugs and determine the possibility of natural products being an important source of future therapeutic agents. Many target-specific anticancer drugs failed to provide successful results, which accounts for a need to investigate natural products with multi-target characteristics to achieve better outcomes. The potential of natural products to be promising novel compounds for cancer treatment makes them an important area of research. This review explores the significance of natural products in inhibiting the various signaling pathways that serve as drivers of carcinogenesis and thus pave the way for developing and discovering anticancer drugs.This study was supported by Sidra Medicine Precision Program funding to Ajaz A. Bhat (5081012003) and Mohammad Haris (5081012002)