Cite
HARVARD Citation
Berger, A. et al. (n.d.). Dolomite microstructures between 390° and 700 °C: Indications for deformation mechanisms and grain size evolution. Journal of structural geology. pp. 144-152. [Online].
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Berger, A. et al. (n.d.). Dolomite microstructures between 390° and 700 °C: Indications for deformation mechanisms and grain size evolution. Journal of structural geology. pp. 144-152. [Online].