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Available results of seismic reflection, refraction and receiver functions studies are assembled in an integrated model at a uniform grid (15\u2032 \u00d7 15\u2032). The model consists of three layers: sediments and two layers of the crystalline crust. Besides depth to the boundaries, we provide average <jats:italic>P<\/jats:italic>\u2010wave velocities in the upper and lower parts of the crystalline crust. The new model demonstrates large differences in the Moho depth compared to previous compilations, over \u00b110 km in some specific areas (e.g. the Baltic Shield). Furthermore, the velocity structure of the crust is much more heterogeneous than in previous maps. EuCRUST\u201007 offers a starting point for numerical modeling of deeper structures by allowing correction for crustal effects beforehand and to resolve trade\u2010off with mantle heterogeneities.<\/jats:p>","DOI":"10.1029\/2007gl032244","type":"journal-article","created":{"date-parts":[[2008,3,13]],"date-time":"2008-03-13T20:16:05Z","timestamp":1205439365000},"source":"Crossref","is-referenced-by-count":222,"title":["EuCRUST\u201007: A new reference model for the European crust"],"prefix":"10.1029","volume":"35","author":[{"given":"Magdala","family":"Tesauro","sequence":"first","affiliation":[{"name":"Netherlands Research Centre for Integrated Solid Earth Science, Faculty of Earth and Life Sciences Vrije Universiteit  Amsterdam Netherlands"},{"name":"GeoForschungsZentrum Potsdam  Potsdam Germany"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Mikhail K.","family":"Kaban","sequence":"additional","affiliation":[{"name":"GeoForschungsZentrum Potsdam  Potsdam Germany"},{"name":"Institute for Physics of the Earth  Moscow Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Sierd A. 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