2023
DOI: 10.1016/j.gloplacha.2023.104090
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Coupled kinematic and thermal modelling of collisional orogens: Implications for subsurface geo-resources assessment in the external Dinarides

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Cited by 2 publications
(1 citation statement)
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“…The Mohorovičić discontinuity, which separates the crust from the upper mantle in the Pannonian Depression is at a shallow depth, so geothermal gradients are higher than in other areas 6.2 to 5.6 ⁰C/100 (Airinei, 1987). This explains the presence of a continuous internal heat source (Demetrescu, 1982;Nader et al, 2023), which is transferred to the underground waters, transforming them into thermal waters. The thickness of the crust is [25][26][27][28][29][30] The numerous faults of the foundation, which also influence the sedimentary cover, favour the rise of geothermal waters.…”
Section: Evaluation Of the Influence Of The Geological Evolution Of T...mentioning
confidence: 99%
“…The Mohorovičić discontinuity, which separates the crust from the upper mantle in the Pannonian Depression is at a shallow depth, so geothermal gradients are higher than in other areas 6.2 to 5.6 ⁰C/100 (Airinei, 1987). This explains the presence of a continuous internal heat source (Demetrescu, 1982;Nader et al, 2023), which is transferred to the underground waters, transforming them into thermal waters. The thickness of the crust is [25][26][27][28][29][30] The numerous faults of the foundation, which also influence the sedimentary cover, favour the rise of geothermal waters.…”
Section: Evaluation Of the Influence Of The Geological Evolution Of T...mentioning
confidence: 99%