<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saitis, G.</style></author><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Kawasaki, S.</style></author><author><style face="normal" font="default" size="100%">Koutsopoulou, E.</style></author><author><style face="normal" font="default" size="100%">Komi, A.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A minerochemical cement study of a beachrock slab: The case study of Peristeria, Salamis Island</style></title><secondary-title><style face="normal" font="default" size="100%">15th International Congress of the Geological Society of Greece</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><pub-location><style face="normal" font="default" size="100%">Athens - Greece</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;Beachrocks are consolidated sedimentary formations and are composed of coastal sediments, which are cemented through&amp;nbsp;the precipitation of carbonates. The lithification takes place in the intertidal zone and can include various sediments, such&amp;nbsp;as sands and gravels of clastic and biogenic origin. This study deals with the cements’ mineralogical and geochemical&amp;nbsp;features of a beachrock outcrop and its aim is the contribution for further understanding on the cementation process of&amp;nbsp;beachrocks. (e.g. Vieira and Ros, 2007; Vousdoukas et al., 2007; Karkani et al., 2017).&lt;/div&gt;</style></abstract></record></records></xml>