Post-Development, a body of transitional imaginaries, is not homogenous, neither in its critique, nor in the alternatives proposed. Given that the term ‘development’ is already highly contentious, the question of what ‘alternatives to development’ might be, becomes difficult to respond to. In this article, we argue that Post-Development can assume many faces that are highly dependent upon their conceptual and geographical contexts. In analysing practices of resistance, contestation and subversion in Tanzania, Iran and Haiti we investigate in what ways various forms of peasant and community organising can be considered transformative and non-hegemonic. In exploring their common ground, we attempt to examine in what ways strategies of reciprocity, solidarity and commoning in different geographical locations and contexts can be understood as means of survival and/or as efforts to provide alternative pathways for societal and economic transformation.

Fractal methods are regarded as a highly efficient method for more accurate separation of boundaries between mineralized zone in shallow and deep studies. In this research, concentration-number (C-N) and concentration-area (C-A) fractal methods were used in order to identify promising areas of the elements like Cr, Co and Ni in the Khoy 1:100.000 geological mapping sheet, NW Iran. The factor analysis was performed on the elements, and factors, which were related to the elements, were isolated and studied by both fractal methods. The current geological locations of the extreme anomalies were investigated and the results showed a very close relationship and overlapping. The results of the presented models show that the most elements under study are located in the central and southwestern parts of the sheet. From the point of view of the lithology, these areas correspond to the serpentinite ultramafic units of harzburgite and dunite, and as a result, there is a high probability of Cr mineralization. The achieved results are confirmed by factor analysis. This means that a factor accumulation of these elements is exactly the same as those of each element.

 1 ، ‫براتی‬ ‫حسین‬ ‫امیر‬ 2 ‫کار‬ ‫لطافت‬ ‫امیر‬ ، 1 ‫جمشیدی‬ ‫اشرف‬ ‫علی‬ ، 3 ‫هوانلو‬ ‫فریبرز‬ ، 4 1 ‫دا‬ ‫ورزشی،‬ ‫شناسی‬ ‫آسیب‬ ‫و‬ ‫بیومکانیک‬ ‫گروه‬ ) ‫ایران‬ ‫تهران،‬ ‫خوارزمی،‬ ‫دانشگاه‬ ‫بدنی،‬ ‫تربیت‬ ‫نشکده‬ 2 ‫ایران‬ ‫تهران،‬ ‫بهشتی،‬ ‫شهید‬ ‫دانشگاه‬ ‫بدنی،‬ ‫تربیت‬ ‫دانشکده‬ ‫ورزشی،‬ ‫شناسی‬ ‫آسیب‬ ‫گروه‬ ) 3 ‫ایران‬ ‫تهران،‬ ‫ایران،‬ ‫پزشکی‬ ‫علوم‬ ‫دانشگاه‬ ‫توانبخشی،‬ ‫علوم‬ ‫دانشکده‬ ‫فیزیوتراپی،‬ ‫گروه‬ ) 4 ‫فیزیولوژی،‬ ‫گروه‬ ) ‫دانشگاه‬ ‫بدنی،‬ ‫تربیت‬ ‫دانشکده‬ ‫ایران‬ ‫تهران،‬ ‫بهشتی،‬ ‫شهید‬

Fractal methods are regarded as a highly efficient method for more accurate separation of boundaries between mineralized zone in shallow and deep studies. In this research, concentration-number (C-N) and concentration-area (C-A) fractal methods were used in order to identify promising areas of the elements like Cr, Co and Ni in the Khoy 1:100.000 geological mapping sheet, NW Iran. The factor analysis was performed on the elements, and factors, which were related to the elements, were isolated and studied by both fractal methods. The current geological locations of the extreme anomalies were investigated and the results showed a very close relationship and overlapping. The results of the presented models show that the most elements under study are located in the central and southwestern parts of the sheet. From the point of view of the lithology, these areas correspond to the serpentinite ultramafic units of harzburgite and dunite, and as a result, there is a high probability of Cr mineralization. The achieved results are confirmed by factor analysis. This means that a factor accumulation of these elements is exactly the same as those of each element.