Different aspects of the geothermics of the Pannonian basin are investigated from the viewpoint of neotectonics. A heat flow map of the basin and the surrounding region is presented. It is shown that the high heat flow of the Pannonian basin, the subsidence and maturation history of the Neogene sediments can be explained in general…
Stephan Mueller special publication series Template
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About the Stephan Mueller special publication series format
Stephan Mueller special publication series is a peer-reviewed journal published by Copernicus Publications, covering Geological and Geochemical Analysis, Geological Formations and Processes Exploration, earthquake and tectonic studies.
| Publisher | Copernicus Publications |
|---|---|
| Reference style | Author–year (Copernicus) Author–year — (Smith, 2023) in the text Smith, A., Jones, B., and Lee, C.: A representative article title, Stephan Mueller special publication series, 12, 45–58, 2023.
Formats any DOI in Stephan Mueller special publication series style. No sign-up. |
| Publishes research in | Geological and Geochemical Analysis Geological Formations and Processes Exploration earthquake and tectonic studies Geological Studies and Exploration High-pressure geophysics and materials |
| Papers published last year | ≈53 |
| ISSN | 1868-4556 |
| h-index | 29 |
| i10-index | 52 |
| Total citations | 2,352 |
| Open access | Yes |
| Top institutions publishing here | Geological Institute |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Most-cited papers in Stephan Mueller special publication series
Geodynamic evolution of the Carpathian arc and Pannonian basin during the Neogene times is presented as a set of palinspastic reconstructions. The structural evolution is modeled in terms of a coupled system of: (1) Alpine (Atype) subduction and compressive orogene belt development owing to compression by the Adriatic microplate, (2) lateral extrusion of Alcapa lithosphere…
Depending on the polarity of the subduction system controlling the evolution of an orogenic wedge, we distinguish between pro-wedge (fore-arc, foreland) and retrowedge (retro-arc, hinterland) forelands. Flexural foreland basins and/or intraplate compressional structures can develop in retro-wedge domains of Andean-type and in pro-and retro-wedge domains of Himalayan-type orogens.
Numerous brittle deformations related to the Late Cretaceous inversion of the Mid-Polish Trough (MPT) have been identified in its various parts using seismic data. The role of Zechstein evaporitic deposits during basin evolution and inversion is also described. A model for the Pomeranian segment of the MPT has been constructed that includes significant decoupling between…