غلام حسین نظری

One of the characteristics and indicators of employees in performing police activities is having professional competencies, considering that police missions are associated with many risks, therefore, in this field, employees must have the necessary competencies. Therefore, the purpose of this research is to design the model of professional competencies of the employees of the police command of the Islamic Republic of Iran (case study: Fateb police).

The research was conducted in terms of purpose, application, qualitative method, and in terms of the nature and type of study using the foundation's data approach (Ground Theory). Government and vice-presidents, managers and heads of vice-departments and specialized departments for dealing with crimes in the intelligence police have formed 15 people with a targeted sampling method. The data collection tool was semi-structured interview and was used to ensure validity from the opinion of expert and knowledgeable professors, and the data was used with the method of content analysis and the use of "Max Kyuda" software.

In the qualitative section, out of 106 primary concepts (open code), 39 main concepts (core code) with 6 dimensions were obtained, which in the form of a paradigm model including a core category with 6 components, causal factors with 3 components, background factors with 8 components. , strategic factors with 8 components, intervening factors with 3 components and consequences with 11 components were presented.

In order to effectively play the key role of employees in Faraja, it is necessary to carry out plans for selection and development of their competencies based on a model that fits the requirements of new competency models. The model presented in this research can be used as a basis in this field.

The purpose of this research is to identify the factors influencing the professional competencies of personnel in the Law Enforcement Force of the Islamic Republic of Iran. The study was conducted with an objective-oriented approach.

The research population consisted of two groups: members of the academic faculty in educational management, higher education, and public administration (who had expertise in professional competencies through books or articles), and the second group included deputies, managers, and heads of specialized departments responsible for handling crimes in the Criminal Police. Fifteen individuals were purposively selected based on theoretical saturation criteria.

Data were collected through semi-structured interviews using MaxQDA12 software. As a result, 106 initial concepts (open codes) and 39 main concepts (core codes) with six dimensions were obtained. These dimensions formed a paradigm model, including: Core Concept with 6 Components. Alienating Factors with 3 Components. Background Factors with 8 Components. Strategic Factors with 8 Components. Interventionist Factors with 3 Components. Consequences with 11 Components.

IntroductionLamprophyres are mesocratic to melanocratic igneous rocks, usually hypabyssal, with a panidiomorphic texture and abundant mafic phenocrysts of dark mica or amphibole (or both) with or without pyroxene, with or without olivine, set in a matrix of the same minerals, and with alkali-feldspar restricted to the groundmass (Woolley et al., 1996). Lamprophyres are frequently associated with orogenic settings and a mantle modified by dehydration of subducted slab (Gibson et al., 1995).
Small outcrops of lamprophyres with Paleozoic to Oligocene age are reported from the central parts of Iran (Torabi 2009 and 2010). The primary magmas of these lamprophyres were derived from decompression melting of the mantle induced by a tensional regime of continental crust (Torabi, 2010). Bayat and Torabi (2011) called the western part of the CEIM (Central-East Iranian Microcontinent) (Anarak to Bayazeh) a “Paleozoic lamprophyric province” and suggested that the lamprophyre magmas were formed by subduction of Paleo-Tethys oceanic crust from the Early to late Paleozoic which resulted in the mantle metasomatism and enrichment.
Lamprophyric dykes and stocks of the Kal-e-kafi area (Central Iran, Northern part of Yazd Block) cross-cut the Eocene volcanic rocks and other older rock units such as Cretaceous limestone. These lamprophyres are mainly composed of hornblende (magnesio-hastingsite), clinopyroxene (diopside) and plagioclase (labradorite to bytownite) as phenocryst, in a matrix of fine to medium grained of the same minerals and orthoclase, apatite, magnetite, chlorite and epidote.
In this paper that is a report on the first study on the calc-alkaline lamprophyres of Central Iran, the petrography and mineral chemistry of calc-alkaline lamprophyric dykes of the Kal-e-kafi area are discussed.
Materials and methodsChemical composition of minerals were conducted at Kanazawa University (Kanazawa, Japan) using the wavelength-dispersive electron probe microanalyzer (EPMA) (JEOL JXA-8800R), with 20kV accelerating potential, 20 nA beam current and a counting time of 40 seconds. Natural minerals and synthetic materials were used as standards. The ZAF program was used for data correction. The Fe3 content of minerals was estimated by stoichiometry. The Mg# and Fe# were calculated as [Mg/(Mgᗭ)], and [Fe2(Fe2)] atomic ratio of minerals, respectively.
Trace element values of phenocrystic clinopyroxene, amphibole and plagioclase were analyzed by LA-ICP-MS (laser ablation-inductively coupled plasma-mass spectrometry) using an ArF 193 nm Excimer Laser coupled to an Agilent 7500S at the Earth Science Department of the Kanazawa University (Japan). The diameter of the analyzed points was 60 micrometers for clinopyroxene and 120 micrometers for amphibole and plagioclase.
Mineral abbreviations are adopted from Whitney and Evans (2010).
Results and DiscussionLamprophyres of the Kal-e-kafi area (Central Iran, West of Yazd Block) are exposed as dykes and stocks which cross-cut the Eocene volcanic rocks and other older rock units such as Cretaceous limestone. Field studies indicate that calc-alkaline lamprophyric dykes of the Kal-e-kafi (east of Anarak) are younger than the other igneous rocks.
According to the results of petrography and mineral chemistry, the mesocratic lamprophyres of Kal-e-kafi area are calc-alkaline spessartite.
Unique values of Al2O3 and TiO2 associated with oscillatory zoning of clinopyroxenes reveal the crystallization of clinopyroxenes during ascending of magma.
Plagioclase phenocrysts are labradorite to bytownite in composition and the plagioclases of matrix are labradorite. Chemical composition diversity of plagioclase indicates the fractional crystallization of these lamprophyres.
Amphibole thermometry estimate average temperature of 860°C and barometry by Anderson and Smith (1995) shows 1.5 to 3 kbars pressure. Clinopyroxene thermobarometry calculate 1150 °C temperature and pressure between 2 to 5 kbars.
The geochemical features and thermobarometry of the Kal-e-kafi spessartite minerals suggest that the primary lamprophyric magma was derived from partial melting of a lithospheric mantle spinel lherzolite. Changes in values of pressure, water content, and Oxygen fugacity during magma ascending lead to oscillatory zoning minerals.
Based on the mineral chemistry, it can be concluded that the Kal-e-kafi lamprophyres were formed in a subduction-related environment by a calc-alkaline magmatism.

There are several complicated factors involved in the smuggling of goods; some of them are related to economic and social issues and some others are related to the relate laws, and the planning strategies. Smuggling goods imposes undesirable effects on the financial and economic organizations of the society and it causes the destruction of financial plans and the allocation of resources. Smuggling goods, sometimes, shuts down the industry. Smugglers attempt to smuggle goods using fake documents and false identities and to do so, they utilize whatever needs possible. Based on these information, we can say that there is some sort of network or organization. This organization has a very useful and effective structure. It also has an extraordinary flexibility, but at the meantime, it is very native, and performs at the local level. In this article, there is an attempt to answer the following questions. How do other countries cope fight against it? How are the smuggling organizations do their operations including providing and smuggling goods in the countries under study? And ultimately how can those who fight against smuggling be paid for their efforts according to the rules and regulations?

The Loghar ophiolite is located in ophiolitic belt of Kabul block (southeast of Afghanistan) and it is a part of Neotethyan ophiolites in Alpine - Himalayan orogenic system with Eocene age. Olivine, orthopyroxene, clinopyroxene and spinel are rock forming minerals of Loghar ophiolite mantle peridotite. Most of the olivines from different rock types are serpentinized but some fresh are present with forsterite composition. Orthopyroxene and clinopyroxene are enstatite (Mg# 0.961-0.972) and diopside (Mg# 0.976-0.999) in composition. The Cr# of vermicular and unhedral spinels of lherzolite and subhedral reddish brown spinels of harzburgite are 0.547 and 0.625 respectively. The Cr# of subhedral to euhedral spinels of dunite is 0.477, induced by high content of Al2O3 and low level of Cr2O3. The Cr# of dark red and euhedral spinel of chromitite is 0.633. The peridotites of the studied area belong to sub-oceanic crust mantle. The low content of Al2O3 in pyroxenes (opx and cpx) and the low amount of Na2O in clinopyroxene indicate high degree of partial melting of mantle peridotites. The chemical composition of minerals in dunites are different from that of lherzolite and harzburgite but present considerable similarity with that of the pillow lavas. The dunites of Loghar mantle peridotite (LMP) do not share features with those derived by partial meltiny, but represent sub lithospheric melt channels.