The Kiskunhalas-NE (KIHA-NE) fractured hydrocarbon reservoir is part of the structurally rather complex crystalline basement of the Great Hungarian Plain. In the course of petrologic and thermometric examinations various rock types of the investigated area have been classified and characterized. There are four basic lithological units in the area. In the lowest structural position orthogneiss is common, which according to its petrographic features is assumed to be identical to the orthogneiss body of the adjacent Jánoshalma (JH) basement high (metamorphic peak temperature T < 580 °C according to Zachar and M. Tóth 2004). The next rock unit upward is the highly mylonitized variety of the orthogneiss with textural features suggesting deformation in an extensional stress regime. In the higher section of the mylonite zone graphitic gneiss mylonite is characteristic, with a peak metamorphic T of 410±45 °C. The lithology in the shallowest position of the area is a graphitic carbonate phyllite, with a T of 375 ± 15 °C. Estimation of the deformation temperature for both mylonitic rocks results in approximately Tdef ∼ 455 °C. All data together suggest that between the top (graphitic carbonate phyllite) and the bottom (orthogneiss) of the ideal rock column there is about 200 °C peak metamorphic temperature deviation. The two extreme metamorphic blocks probably became juxtaposed along an extensional fault zone in the basement at approximately 15 km depth.
dilatometric glass-transition temperature ( T g ), deformationtemperature ( T d ), and coefficient of thermal expansion (CTE) were estimated from thermo-mechanical analysis of the samples. The cubes of glasses 5 × 5 × 5 mm were heated (the heating rate of 10 K
The effect of the deformation temperature on the energy stored in post-yield deformed poly(butylene terephthalate) PBT, was
studied by means of DSC tests. Deformed specimens were rapidly cooled after unloading, in order to avoid the energy relaxation
processes occurring before the DSC measurements. Cooling revealed to have a significant contribution on the whole stored energy,
as shown by DSC tests conducted on undeformed PBT specimens conditioned at various temperatures. This work is aimed at separating
the effects due to cooling and those ascribed to deformation on the energy storage and release processes, permitting to better
understand previous findings on post-yield compressed PBT.
Authors:Slobodan Stojadinovic, Jasmina Pekez and Nikola Bajic
on the basis of keeping unrecrystallized (polygonized) structure originates as the consequence of: (a) adding transitional elements, as Mn, Ti and Zr in micro quantity and (b) suitable speed of deformation (low) and deformationtemperatures (high