File:Cycle émersif Maroc.jpg

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Original file(2,359 × 1,647 pixels, file size: 2.43 MB, MIME type: image/jpeg)

Summary

"Shallowing upward" metric sequence of autocyclic origin in the carbonate platform of middle Lias age in the High Atlas Mountains of Morocco. Lagoonal to intertidal deposit with algal mats; early diagenesis, dolomitization (in yellow) in a supratidal environment on top, with tidal and hurricanes deposits, floated foraminifera and breccias (Davaud & Septfontaine, 1995).

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current03:36, 8 January 2017Thumbnail for version as of 03:36, 8 January 20172,359 × 1,647 (2.43 MB)127.0.0.1 (talk)"Shallowing upward" metric sequence of autocyclic origin in the carbonate platform of middle Lias age in the High Atlas Mountains of Morocco. Lagoonal to intertidal deposit with algal mats; early diagenesis, dolomitization (in yellow) in a supratidal environment on top, with tidal and hurricanes deposits, floated foraminifera and breccias (Davaud & Septfontaine, 1995).
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