INTRODUCCIÓNEn este trabajo vamos a desgranar cuales deben ser, en nuestra opinión, los elementos esenciales para desarrollar una psicoterapia de orientación feminista en la atención a las mujeres (y sus hijos/as) que han padecido violencia de gé-nero y, particularmente, violencia en la pareja.En este sentido, cabe recordar que hoy en día la consideración más asumida es que la violencia contra las mujeres es un fenómeno multicausal que sólo puede ser explicado a partir de la intervención de un conjunto de elementos diversos, incluyendo factores individuales, sociales y del contexto concreto 2 . Pero, incluso si hablamos de múltiples causas, en la base de esta pirámide causal encontraríamos una concepción sexista de los agresores, estrechamente ligada a la exacerbación del modelo masculino tradicional (que incluye la consideración de lo masculino como superior, la legitimidad de la supeditación femenina al varón,...) y una estructura social económica y familiar patriarcal que implica una distribución desigual del poder que impregna la construcción social del género y de la sexualidad y que afecta profundamente a las relaciones entre los hombres y las mujeres 3 .
This study focused on analyzing the petroleum system of the Bannu Basin, which is the foreland basin of the Himalayan fold and thrust belts in Pakistan. The objectives of this study were achieved by dividing the study area into three zones, namely, the Southwestern zone, Southeastern zone, and Northeastern zone. The regional 2D seismic lines and well log data, including the bore hole temperature (BHT) and petrophysical and geochemical data, were integrated. The seismic interpretations and geohistory plots indicate higher levels of sedimentation and abrupt sedimentation from the Miocene until the Recent era due to the initiation of Himalayan orogeny. The thermal modeling indicates that potential source rocks are present in the basin, whereas the local faults in the Southwestern and Southeastern zones act as potential traps for the preservation of hydrocarbons. It is assumed that the Tredian Formation and Lumshiwal Formation are the potential reservoir rocks in the Southwestern zone, whereas the Warcha Formation and Tredian Formation are the economic reservoirs in the Southeastern zone. However, in the Northeastern zone, no major accumulation is present. The significant sedimentation of post-Miocene formations was the major event for the generation of hydrocarbons and a critical moment for the accumulation of hydrocarbons in the study area.
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