Syn-kinematic sedimentary systems as constraints on the structural response of thrust belts: re-examining the structural style of the Maghrebian thrust belt of Eastern Sicily
Author(s) -
Robert W. Butler,
Rosanna Maniscalco,
Patricia R. Pinter
Publication year - 2019
Publication title -
italian journal of geosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.584
H-Index - 37
eISSN - 2038-1727
pISSN - 2038-1719
DOI - 10.3301/ijg.2019.11
Subject(s) - geology , anticline , fold and thrust belt , sedimentary depositional environment , paleontology , thrust , neogene , sedimentary rock , tectonics , accretionary wedge , seismology , thrust fault , structural basin , foreland basin , subduction , physics , thermodynamics
We are indebted to the generosity of the late Fabio Lentini. While he may not have agreed with our findings, he nevertheless openly and cheerfully shared his mapping and insight of Sicilian geology. This work also builds upon many years’ collaboration between us, initiated by the late Mario Grasso (the Pantagruelian Master of Speranza et alii, 2018). The mapping of Lentini, Grasso and colleagues represents a remarkable resource for future geologists. We dedicate this contribution to their memory. We thank Sveva Corrado and an anonymous referee for constructive comments on an earlier draft of this paper. Butler’s Sicilian field research has been variously funded by the UK’s Natural Environment Research Council and the Royal Society. Maniscalco acknowledges “Fondi per la Ricerca di AteneoPiano per la Ricerca 2016/2018”. Pinter was supported through a PhD grant funded by the BG Group (now Shell) and Brazil’s National Council for Scientific and Technological Development (CNPq).
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