2023
DOI: 10.1016/j.gloplacha.2023.104090
|View full text |Cite
|
Sign up to set email alerts
|

Coupled kinematic and thermal modelling of collisional orogens: Implications for subsurface geo-resources assessment in the external Dinarides

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2023
2023
2023
2023

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(1 citation statement)
references
References 84 publications
0
1
0
Order By: Relevance
“…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%