Fig. 7

Download original image
The fine facies grained of the Douleb Member (Units U2 and U3). A: (Mf10) Anhydrite facies. B: (Mf4) Stylolitic packstone with calcispheres (a) and planktonic foraminifera (b), the calcispheres are filled with pyrite, (c) phosphatization of the matrix. C: (Mf12) Sandy packstone with calcispheres (a) and planktonic foraminifera (b), quartz (c). D: (Mf5) Stylolitic packstone with miliolids (a), benthic and planktonic foraminifera (b), phosphatisation (c). E: (Mf8) Two microfacies: 1 a stylolitic packstone rich in oolites (a), echinoderms (b), planktonic foraminifera (c), gastropods and micritized bioclasts, 2 wackestone-packstone rich in echinoderms and foraminifers. F: (Mf8) Oolitic packstone intercalated by a grainstone texture microfacies with small pellets (a) and stylolites (b).
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.