<?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%">Petropoulos, A.</style></author><author><style face="normal" font="default" size="100%">Baziotis, I.</style></author><author><style face="normal" font="default" size="100%">Anagnostou, C.</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></authors></contributors><titles><title><style face="normal" font="default" size="100%">Beachrocks cement characteristics and conditions of formation. Case study Platanias beach, Chania, Greece.</style></title><secondary-title><style face="normal" font="default" size="100%">14th International Conference of the Geological Society of Greece</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><publisher><style face="normal" font="default" size="100%">Bulletin of the Geological Society of Greece</style></publisher><pub-location><style face="normal" font="default" size="100%">25-27 May, Thessaloniki</style></pub-location><volume><style face="normal" font="default" size="100%">L</style></volume><pages><style face="normal" font="default" size="100%">458-467</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;Beachrocks represents a coastal deposition in the intertidal area, and studying their&amp;nbsp;properties may lead to create a model which identifies the conditions of their&amp;nbsp;formation (paleo-environment). This paper focuses most intently on the cement&amp;nbsp;material which is able to recover the paleo-environment conditions during diagenesis&amp;nbsp;of such coastal sediment. We used optical microscopy, secondary electron microscopy&lt;/div&gt;
&lt;div&gt;and Raman Spectroscopy to characterize the cement texture, mineralogy and&amp;nbsp;chemistry in the beachrocks. The existence of pure calcite primarily controlled by the&amp;nbsp;meteorite water, while Mg-calcite appears between the lower meteoric and the upper&amp;nbsp;marine phreatic zone. Finally, the presence of aragonite associated with the marine&amp;nbsp;phreatic to lower marine vadose environment.&lt;/div&gt;</style></abstract></record></records></xml>