<!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>SINTEMA DI BACCINELLO-CINIGIANO</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">BAB</SPAN></B><B><SPAN CLASS="f1">a</SPAN></B><B><SPAN CLASS="f1"><BR></SPAN></B><B><SPAN CLASS="f1">Litofacies </SPAN></B><B><SPAN CLASS="f1"> marnoso - </SPAN></B><B><SPAN CLASS="f1">calcarea</SPAN></B><B><I><SPAN CLASS="f1"><BR></SPAN></I></B><SPAN CLASS="f1 cl1">Marne e marne calcaree grigio-azzurre e biancastre, bioturbate, spesso siltose e micacee a stratificazione media generalmente poco evidente. Questa litofacies generalmente costituisce la base della formazione. Passa verso lalto ad una litofacies marnoso-arenacea (BABb), talora con passaggio stratigrafico netto e a luoghi con marcate interdigitazioni.</SPAN><SPAN CLASS="f1 cl1"><BR></SPAN><SPAN CLASS="f1 cl1">La potenza affiorante supera i 150 metri.<BR></SPAN><P CLASS="jus"><I><SPAN CLASS="f1">SERRAVALLIANO INF .- TORTONIANO</SPAN></I><I><SPAN CLASS="f1 cl1"><BR></SPAN></I><P CLASS="lft"> <BR></BODY></HTML>