a. najafzadeh

Afghanistan is a country with diverse ethnic minorities that have been in conflict with each other, without much emphasis on nationalism. Lack of social cohesion has led to the dominance of tribal leaders in the country. On the other hand, modern nation-state building has been introduced through the French Revolution and colonization in India. These two ideologies have resulted in a cultural shock, tug of war between tradition and modernity, and violence in Afghanistan. Nationalism, which introduces traditional values into modern clothing, is in conflict with liberalism, which emphasizes post-enlightenment ideology and development in Europe, but has not been able to bring development to Afghanistan. Nationalism has led to division and animosity between the various cultures and ethnic groups in Afghanistan, resulting in social conflicts, weak nationalism, and underdevelopment. Armed uprisings, the emergence of terrorist groups, foreign intervention, the destruction of infrastructure, and the collapse of the developmental mindset are some of the consequences of this underdevelopment. This sociological-historical research aims to answer the question of how the delay in the formation of nationalism affected the development and led to the collapse of the developmental mindset in Afghanistan. The hypothesis is that the delay in the formation of civic nationalism, weak separation of private and public spheres in the eighth constitutional law, lack of historical background to liberal teachings, the non-sociological function of global society, and continuous ethnic nationalism without regard to the past have contributed to this collapse.

In this study, a combination of petrographic and major element geochemistry of siliciclastic deposits of Lower Permian Doroud Formation in the Zal section in south of Jolfa has been used to investigate the provenance, tectonic setting and paleo-weathering. The thickness of Doroud Formation in Zal section is 112 m consisting of micro conglomerate, red sandstone and shale. Thirteen samples of sorted and medium grained sandstones were examined by point-counting method and 6 samples were examined for determination of their major elements by X-ray fluorescence (XRF) method. The studied samples are frequently sublithic-arenite in composition. The study of the amount and type of monocrystalline and polycrystalline quartz and using of discrimination function, indicate that the parent rocks of these deposits are predominantly metamorphic, felsic igneous rocks as well as sedimentary recycled. The presence of chert in petrographic studies has also confirmed the effect of sedimentary recycling from older formations. Petrographic and geochemical studies also indicate the cratonic origin and tectonic setting of the passive continental margin at the time of sediment deposition of the Doroud Formation. Determination of chemical index of alteration (CIA) indicates intense weathering and humid climate in the provenance area, which is consistent with the paleogeography of the Iran in Permian. It seems that factors such as the a long-distance transport on the Arabian Craton, the recycling of older formations and also the humid climate at the time of the deposition of the Doroud Formation, together, have played significant role at the relatively high maturity of this sandstones.