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However, field structural relationships indicate that migmatization occurred synchronously with the emplacement of the quartz dioritic magmas at <jats:italic>c<\/jats:italic>. 299 Ma. Thus, the results of this study suggest that subduction-related calc-alkaline magmatic activity in the Cap de Creus was coeval and coupled with D<jats:sub>2<\/jats:sub> dextral transpression involving NNW\u2013SSE crustal shortening during Late Carboniferous \u2013 Early Permian time (<jats:italic>c<\/jats:italic>. 299\u2013291 Ma). Since these age determinations are within the range of those obtained for undeformed (or slightly deformed) calc-alkaline igneous rocks from NE Iberia, it follows that the Cap de Creus massif would represent a zone of intense localization of D<jats:sub>2<\/jats:sub> transpression and subsequent D<jats:sub>3<\/jats:sub> ductile wrenching that extended into the Lower Permian during a transitional stage between the Variscan and Cimmerian cycles.<\/jats:p>","DOI":"10.1017\/s0016756814000041","type":"journal-article","created":{"date-parts":[[2014,3,11]],"date-time":"2014-03-11T14:03:06Z","timestamp":1394546586000},"page":"1095-1114","source":"Crossref","is-referenced-by-count":54,"title":["Zircon geochronology of intrusive rocks from Cap de Creus, Eastern Pyrenees"],"prefix":"10.1017","volume":"151","author":[{"given":"ELENA","family":"DRUGUET","sequence":"first","affiliation":[]},{"given":"ANTONIO","family":"CASTRO","sequence":"additional","affiliation":[]},{"given":"MARTIM","family":"CHICHORRO","sequence":"additional","affiliation":[]},{"given":"M. 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