h5. Litharenitic Sand, Jura Creek, Rocky Mountains
| !Jura_Creek_CAN_Scen.jpg|thumbnail! | | !Jura_Creek_makro.jpg|thumbnail! |
| Jura Creek \\
{table-cell:width=30%}
{table-cell} | grayGrey, subrounded carbonates |
| *Location* \\ | Jura Creek E of Canmore, Rocky Mountains, Alberta, Canada |
| *Depositional facies* \\ | _replace this with text about the dep facies_ |
| *Provenance* \\ | Geographically narrow provenance in drainage area of Jura Creek, exclusively from devonian limestones and dolomites of the Front Range |
| *Composition* \\ | Dolomite, limestone, shale, some chert, few phosphorite grains |
| *Texture* | _replace this with text about texture_ Coarse sand, very poorly sorted to poorly sorted, angular to subangular |
h6. Petrographic thin section:
| *Description* | Variable fine to coarse, sparry, recrystallised dolomite, few foliated shales, some chert and rare brown phosphorite grains |
| !Jura_Creek_BF.jpg|thumbnail! | | !Jura_Creek_ts_x_sm1200DF.jpg|thumbnail! |
| Bright field \\
{table-cell:width=30%}
{table-cell} | Dark field |
h6. Texture:
coarse sand, very poorly sorted to poorly sorted, angular to subangular
|| *Sample number \\* || Collectorheubeck0060 || Date of sampling \\ ||
| heubeck0060*Collector* | Christoph Heubeck, Institut für Geologische Wissenschaften, FU Berlin |
| *Date of sampling* | August 2005 |
h6. Comments:
Jura Creek is a popular hiking trail east of Canmore and leads to an outcrop of late devonian anoxic shales (Exshaw Shale)
[Additional data page|geowisssand:0060 Additional data]
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