<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Salminen, Johanna</style></author><author><style face="normal" font="default" size="100%">Dinis, Jorge</style></author><author><style face="normal" font="default" size="100%">Mateus,Octávio</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Rogério Rocha, João Pais, José Carlos Kullberg, Stanley Finney</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal</style></title><secondary-title><style face="normal" font="default" size="100%">STRATI 2013 First International Congress on Stratigraphy At the Cutting Edge of Stratigraphy</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><related-urls><url><style face="normal" font="default" size="100%">https://docentes.fct.unl.pt/sites/default/files/omateus/files/salminen_et_al_2014_porto_da_calada_stratigraphy_jk_boundary_in_rocha_et_al_strati_.pdf</style></url></related-urls></urls><publisher><style face="normal" font="default" size="100%">Springer</style></publisher><pub-location><style face="normal" font="default" size="100%">Heidelberg New York Dordrecht London</style></pub-location><pages><style face="normal" font="default" size="100%">873-877</style></pages><abstract><style face="normal" font="default" size="100%">&lt;p&gt;We present a stratigraphic log supporting a preliminary magnetostratigraphy of a Tithonian–Berriasian section in Porto da Calada (Portugal). Based on biostratigraphy and reversed and normal magnetostratigraphy, the location of the Tithonian–Berriasian boundary is tentatively located at ca. 52 m, not in disagreement&lt;br /&gt;
with former proposals. Due to the occurrence of later remagnetization (diagenesis), the magnetostratigraphic definition of the Tithonian–Berriasian section at the Cabo Espichel (Portugal) location was not able to be established.&lt;/p&gt;
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