SUP18342
Geological Society Supplementary Publication No. SUP18342
Parent Paper: The Shanderman eclogites: a Late Carboniferous high-pressure event in the NW Talesh Mountains (NW Iran).
S. Zanchetta, A. Zanchi, I. Villa, S. Poli & G. Muttoni
Appearing in The Geological Society, London, Special Publications, 312, 57–78.
Tables are provided presenting various forms of data within .csv files.
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Table 1. GPS coordinates of analyzed samples.
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Table 2. Whole rock chemical data (major and trace element) of intrusive rocks and metabasites of the Shanderman Complex.
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Table 3. Representative electron microprobe analyses of garnet from Shanderman eclogites.
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Table 4. Chemical composition of omphacite from Shanderman eclogites.
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Table 5. Representative electron microprobe analyses of phengite and paragonite from Shanderman eclogites.
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Table 6. Amphibole chemical compositions from Shanderman eclogites.
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Table 7. Representative chemical compositions of epidote and clinozoisite from Shanderman eclogites.
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Table 8. Representative electron microprobe analyses of chlorite, titanite and plagioclase from Shanderman eclogites.
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Table 9. Chemical compositions of garnet and clinopyroxene pairs employed for geothermometry.
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- Table 10. Thermometric estimates on grt-cpx pairs from samples IR24 and RA32 (numbers in brackets refer to Tab. 9 compositions). (.csv0 Kb)





