Transformation of echinoid Mg calcite skeletons by heating
Interambularcral plates of echinoid Heterocentrotus trigonarius, composed of Mg calcite 1 (≈14 mol% MgCO 3), were heated in three timed series of experiments at 300°C. Dried plate fragments and fragments with added water were heated separately in pressurized bombs. X-ray powder diffractometry, unit...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2001-02, Vol.65 (3), p.443-454 |
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