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Publikováno v:
Journal of Volcanology and Geothermal Research. 336:155-167
The ultimate shape of a laccolith is the result of competition between internal magmatic phenomena (e.g. overpressure and the process of solidification), and the state of the external host rock (e.g. thickness of the overburden, the presence of fault
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4fde053ba7f1bc112ac6c2e6fbee61b2
https://doi.org/10.1016/j.jvolgeores.2017.02.017
https://doi.org/10.1016/j.jvolgeores.2017.02.017
