<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.01 Strict//EN"><HTML><HEAD><META HTTP_EQUIV="Generator" CONTENT="RTF 2 HTML Converter 0.2, (C) Sergey A. Galin, 2001-2002"><META HTTP-EQUIV="Content-Type" CONTENT="text/html; charset=Windows-1252"><title>a1</title><META HTTP-EQUIV="Author" CONTENT="nuccia"><!-- Operator: fabiana --><!-- Company: cgt --><STYLE TYPE="text/css"><!--p margin: 0; table border-collapse: collapse; border: none; td border: solid 1px black; .lft text-align: left; .rgt text-align: right; .cen text-align: center; .jus text-align: justify; .wn font-weight: normal; .sn font-style: normal; .u text-decoration: underline; .lst font-family: Wingdings, fantasy; .strike text-decoration: line-through; .sz9 font-size: 9pt; .f0 font-family: Times New Roman, Times, serif; .f40 font-family: Times, serif; .f1 font-family: Arial, sans-serif; body font-size: 12pt; color: black; background-color: white; @f0; --></STYLE></HEAD><BODY><P CLASS="jus f40 sz9"><B><SPAN CLASS="f1 cl1">DSA</SPAN></B><B><SPAN CLASS="f1 cl1"><BR></SPAN></B><P CLASS="lft"><B><SPAN CLASS="f1">DIASPRI DI MONTE ALPE</SPAN></B><B><SPAN CLASS="f1"><BR></SPAN></B><SPAN CLASS="f1">Radiolariti e selci rosse, grigie, o grigio verdi, in strati sottili, a cui si intercalano argilliti silicee rosse e nere, prevalenti nella porzione superiore della formazione; nella porzione inferiore sono presenti inoltre brecciole, areniti e siltiti ofiolitiche e in quella sommitale rare marne siltose grigie, calcilutiti silicee e brecce ad elementi silicei.</SPAN><SPAN CLASS="f1"><BR></SPAN><I><SPAN CLASS="f1">BAJONCIANO SUPERIORE/BATHONIANO INFERIORE-</SPAN></I><I><SPAN CLASS="f1"><BR></SPAN></I><I><SPAN CLASS="f1">?BERRASIANO SUPERIORE/VALANGINIANO INFERIORE</SPAN></I><I><BR></I><BR><BR></BODY></HTML>