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- W2810367339 abstract "Romania hosts some of the largest salt deposits in Europe, most of them located in the Eastern Carpathians and the Transylvania Depression. These are thick Miocene age evaporates precipitated in a lagoon facies. Since the end of the eighteenth century, geologist extensively mapped the salt deposits for mining purposes, gaining worldwide recognition. In fact, the term diapir was introduced in the geological literature by the Romanian scientist Ludovic Mrazec in 1906. The karst formed on evaporite rocks represents about 5% of the Romania’s exposed karst and is located mostly in the lowland hills of Eastern Subcarpathians Bend. The salt outcrops on ~150 km2, just 0.06% of Romanian territory. A few details about Meledic Plateau, which is part of the Buzău Land Geopark, and the Slănic Prahova Salt Mine, are the subject of this brief chapter." @default.
- W2810367339 created "2018-07-10" @default.
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- W2810367339 date "2018-07-05" @default.
- W2810367339 modified "2023-09-25" @default.
- W2810367339 title "Eastern Subcarpathians Bend: Salt Karst: Meledic Plateau and Slănic Prahova" @default.
- W2810367339 cites W2540319985 @default.
- W2810367339 doi "https://doi.org/10.1007/978-3-319-90747-5_51" @default.
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