Dolomite is easily recognised from its shape and chemical composition. I have a problem in determining and differenciating crystals thought to be dolomite and/or high Mg calcite (HMC). These are very old carbonates (Late Cret age) and most of the crystals show inclusions and are either euhedral or subhedral-anhedral, they also show high peaks of Mg on EDX. No doubt, these are dolomites....BUT! other crystals (which are cements) are very clean, no inclusions, are planar subhedral-anhedral and show some high Mg peaks on EDX; some are nonplanar too. As old as they are, I would hardly think they are HMC's. Is it possible to find clean sparry crystals (as cements) with the above features to be dolomite? Any ideas? Thanks
2007-03-14
20:40:59
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3 answers
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too good to be true
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Science & Mathematics
➔ Earth Sciences & Geology
Thank you all for the wonderful answers to my question. They were helpful in aome way.
Mr. Scientist, I agree XRD is still a good technique and that is how I got peaks of Mg of different levels. None of the crystals show only MgCo3; very low peaks of Fe, Si and ocassionally K, occur. I think HMC is metastable and cannot resist diagenesis for such a time.
Actually, it's not a single mineral but a lake carbonate rock with lots of microbial structures in the matrix. From the planar subhedral crystals and inclusions in them, I thought they were originally calcites that got dolomitized during diagenesis. But these inclusions also show high Mg peaks from XRD...I wonder?
Thanks again for the wonderful answers....I am enjoying this exchange of knowledge and welcome input from anybody.
2007-03-16
03:36:23 ·
update #1
Thank you all for the wonderful answers to my question. They were all helpful in some way.
Mr. Scientist, I agree XRD is still a good technique and that is how I got peaks of Mg of different levels. None of the crystals show only MgCo3; very low peaks of Fe, Si and occassionally K, occur. I think HMC is metastable and cannot resist diagenesis for such a time.
Actually, it's not a single mineral but a lake carbonate rock with lots of microbial structures in the matrix. From the planar subhedral crystals and inclusions in them, I thought they were originally calcites that got dolomitized during diagenesis. But these inclusions also show high Mg peaks from XRD...I wonder?
Thanks again for the wonderful answers....I am enjoying this exchange of knowledge and welcome input from anybody.
2007-03-16
03:39:00 ·
update #2