Abstract
The second world occurrence for jinshajiangite has been encountered at Norra Kärr, where the mineral appears as tabular grains up to 4 mm long, essentially in albite veinlets. Associated phases are, inter alia, magnesio-arfvedsonite, aegirine, fluorapatite and rosenbuschite. Refinement of the monoclinic unit-cell parameters gave a = 10.696(2) Å, b = 13.800(5) Å, c = 20.705(3) Å, β = 94.96(2)° and V = 3044.7(5) Å3. The Norra Kärr jinshajiangite is chemically distinguished from the type material mainly by a higher Fe2+/(Fe2+ + Mn) ratio. It is interpreted as a late-magmatic product related to fractionation.