Figure 7
From: Carbonation and serpentinization of diopsidite in the Altun Mountains, NW China
Chondrite- and primitive mantle-normalized diagrams. (a, b) Fresh diopsidites and diopsides; (c, d) diopside relics; (e, f) serpentines after diopsides and in late veins; (g, h) calcites after diopsides and in late veins. The (a-c-e–g) and (b-d-f–h) patterns are chondrite- and primitive mantle-normalized, respectively; normalizing values are from McDonough and Sun47. Blue fonts indicate fluid-mobile elements (FMEs). Grey and pink lines represent the values for the studied serpentinized diopsidite and the average value for diopside relics, respectively.
