Porta, Jaime deCivis-Llovera, Jorge2017-03-082017-03-081995http://hdl.handle.net/10272/13416According to the micropaléontological and macropaleontological data, the Penedès Miocene marine sediments, and the Tarràgoha-Bonastre horst, represents Langhian and Langhian to Serravallian-Tortonian ages, respectively. The N 8 to N 16 biozones (Blow, 1969) have been recognized. According to these data, the marine sedimentation in the Penedès area finished in the LanghianspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/ForaminiferaPectihidsBiostratigraphyNeogeneMediterranean SystemLa sucesión bioestratigráfica del Mioceno marino en el Penedés y en el hörst de Tarragona-Bonastre (Neógeno del Sistema Mediterráneo)Biostratigraphic sequeríce of the marine Miocene in the Penedés and Tarragona-Bonastre hörst (Mediterranean System)journal articleopen access