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Comment on Maravelis et al. “Accretionary prism-forearc interactions as reflected in the sedimentary fill of southern Thrace Basin (Lemnos Island, NE Greece)”

Comment on Maravelis et al. “Accretionary prism-forearc interactions as reflected in the sedimentary fill of southern Thrace Basin (Lemnos Island, NE Greece)” Thumbnail


Abstract

This contribution is intended to shed light on the content of the paper by Maravelis et al. (2015) about the evolution of the island of Limnos, a small portion of the Cenozoic Thrace Basin (Turkey, Greece and Bulgaria). Although we appreciate their approach to use sediment provenance for paleotectonic reconstructions, we have concerns how this subject has been dealt with and how it is presented to the scientific community. Most of our criticism is about the attempt of Maravelis et al. to provide a review of the evolution of the Thrace Basin using (1) an inadequate dataset, (2) an inadequate area (Limnos is <5 % of the Thrace Basin) and (3) the interpretation provided by different authors in previous papers without properly citing the source of the information.

Acceptance Date Jan 19, 2016
Publication Date Jan 1, 2017
Journal International Journal of Earth Sciences
Print ISSN 1437-3254
Publisher Springer Verlag
Pages 387 -388
DOI https://doi.org/10.1007/s00531-016-1302-7
Keywords Continental Crust; Accretionary Prism; Lithic Fragment; Volcanic Material; Trace Element Data
Publisher URL http://dx.doi.org/10.1007/s00531-016-1302-7

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