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Published in 2018 at "International Journal of Earth Sciences"
DOI: 10.1007/s00531-018-1619-5
Abstract: The Jurassic pillow basalt of the NE Hungarian Szarvaskő Unit is part of an incomplete ophiolitic sequence, formed in a back-arc- or marginal basin of Neotethyan origin. Different, often superimposing hydrothermal processes were studied aiming…
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Keywords:
geotectonic evolution;
hydrothermal processes;
szarvask unit;
szarvask ... See more keywords