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Publikováno v:
Carbonates and Evaporites. 34:389-403
Dolomites are well-known minerals; belonging to the Infra-Cambrian Hormuz Series lies within the salt domes of southern Iran. In this paper, the origin and alteration of dolomitic rocks of Paskhand and Deh-kuyeh salt diapirs in the area of Larestan (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88d93de1332dcb9d2aeee6d494cddab6
https://doi.org/10.1007/s13146-017-0399-5
https://doi.org/10.1007/s13146-017-0399-5
