--> Figure

Datapages, Inc.Print this page

Figure. 2.10. Anhydrite filled relict porosity in pisolitic bioclastic grapestone grainstone. The original isopachous cements fringing the pore have been dolomitized along with the rest of the carbonates in this section. Left - plane light; Right - crossed polarizers. Gissler B #29, 1911.4 feet depth, LA = 0.38 mm.