<?xml version="1.0" encoding="UTF-8"?>
<references>
<reference>
  <a1>Alçiçek, M.C.</a1>
  <a2>Alçiçek, H.</a2>
  <a2>Altunel, E.</a2>
  <a2>Arenas, C.</a2>
  <a2>Bons, P.</a2>
  <a2>Brogi, A.</a2>
  <a2>Capezzuoli, E.</a2>
  <a2>de Riese, T.</a2>
  <a2>Porta, G.D.</a2>
  <a2>Gandin, A.</a2>
  <a2>Guo, L.</a2>
  <a2>Jones, B.</a2>
  <a2>Karabacak, V.</a2>
  <a2>Kershaw, S.</a2>
  <a2>Liotta, D.</a2>
  <a2>Mindszenty, A.</a2>
  <a2>Pedley, M.</a2>
  <a2>Ronchi, P.</a2>
  <a2>Swennen, R.</a2>
  <a2>Temiz, U.</a2>
  <t1>Comment on “First records of syn-diagenetic non-tectonic folding in Quaternary thermogene travertines caused by hydrothermal incremental veining” by Billi et al. Tectonophysics 700–701 (2017) 60–79</t1>
  <t2>Tectonophysics</t2>
  <sn/>
  <op/>
  <vo/>
  <ab/>
  <la>eng</la>
  <k1/>
  <pb/>
  <pp/>
  <yr>2017</yr>
  <ed/>
  <ul>http://zaguan.unizar.es/record/74872/files/texto_completo.pdf;
	http://zaguan.unizar.es/record/74872/files/texto_completo.jpg?subformat=icon;
	</ul>
  <no>Imported from Invenio.</no>
</reference>

</references>