The symbolistic poetry of Alexander Blok is connected with the thinking of both philosophers and psychoanalysts about the world and the man inscribed in it by the phenomenon of “I”. When coming into contact with transcendence, the poet crosses the demarcation line dividing the rational and irrational world, consciousness and unconsciousness. In the first period of creativity, the Russian symbolist nourishes his imagination, infl uenced by the philosophy of Vladimir Soloviev, with longing for the ideal of femininity. The driving force of the Blok’s imagination becomes, understood after Freud, the desire to meet the ideal residing in the oneiric space, and then to unite with it at the dual level (physical and spiritual). From the psychoanalytic perspective, the cycle Verses about the Beautiful Lady is both an attempt to go beyond awareness and search for the sense of a poetic image, its original source in the unconscious, as well as entering into the mirror phase described by J. Lacan. Beautiful Lady plays a role of what the French psychiatrist appoints as an objet petit a: this object is essentially unreachable and that is why it raises a great desire in the lyrical subject. The mechanism of the transition from chaos to unity, though only apparent in Blok’s works, is identical to the psycho-physical experience of the child, observing himself in the mirror.
The results of drill stem tests made on the autochthonous Miocene deposits of the Upper Badenian - Lower Sarmatian age in the Carpathian Foredeep were analyzed. Reservoir tests were performed in open and cased holes, where inflows of formation water of varying saturation degree and sometimes contaminated with drilling mud filtrate, were observed. A total of 58 intervals, geophysically qualified as gas-bearing, were analyzed. Statistical analysis methods were used for determining the influence of the formation depth on the depth of deposition of the Miocene, and also dependence of initial back-pressure exerted on the reservoir during DST, on the depth of deposition of the reservoir. No correlation was found between water flow rate and initial differential pressure. A satisfactory correlation was obtained between hydrostatic pressure of water cushion in the tubing string and reservoir pressure for selected 22 the Miocene intervals in the Dębica region. In this region the pressure quotient php/pz broadly ranged between 0.05 and 0.57. Another correlation was noted between initial back-pressure and a depth at which pressure was measured and initial back-pressure, and formation water flow rate. The regression equations determined with statistical methods can be used for predicting values of formation pressure, initial value of back-pressure, formation water flow rate and initial differential pressure during DST. On this basis technological parameters of successive reservoir tests can be determined for in the analyzed area of the Carpathian Foredeep, particularly in the Dębica region.