File:Sandstone homoaxial cement.jpg
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| Description | Thin section of the Weverton quartzite/sandstone (Cambrian of Maryland, USA), cross polarized light. All crystals are of the mineral quartz. The original rounded shape of the detrital grains is preserved in fluid inclusion patterns. A homoaxial cement of quartz grew into the pores untill the whol rock was cemented. |
| Date | |
| Source | Own work |
| Author | Woudloper |
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I, the copyright holder of this work, release this work into the public domain. This applies worldwide. In some countries this may not be legally possible; if so: I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 09:54, 22 December 2007 | | 1,600 × 1,200 (924 KB) | Woudloper (talk | contribs) | {{Information |Description=Thin section of the Weverton quartzite/sandstone (Cambrian of Maryland, USA), cross polarized light. All crystals are of the mineral quartz. The original rounded shape of the detrital grains is preserved in fluid inclusion patte |
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