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Title: Petrogenesis of kornerupine at the classic locality of Waldheim, German Democratic Republic

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6596617

The Waldheim kornerupine rock (Sauer, 1886), a 3 x 15m lens in the Saxony granulites, consists of an Na-oligoclase (Pl) matrix containing rutile (Rt), biotite (Bt), corundum (Crn), sapphire (Spr), kyanite (Ky), sillimanite (Sil), andalusite (And), kornerupine (Krn), tourmaline (Tur), dumortierite (Dum), and zoned garnet (Grt). Newly collected samples and chemical analyses, together with literature data (mostly Kalkowsky, 1907; Scheumann, 1960; Schreyer, Abraham, and Behr, 1975) are used to propose a petrogenetic model for the kornerupine rock. A suggested precursor is an Na-rich sediment into which boron had been introduced by exhalative processes or by an evaporite brine. Boron contents are Tur (11.7), Krn (3.40), Spr (0.81), Sil (0.32), Pl (0.02), Bt (0.004), and Ky(0). Ion microprobe fluorine contents (weight %) are Krn (0.73), Bt (2.7), and Tur (0.77) and lithium (as oxide), Krn (0.12), Bt (0.10), and Tur (trace). Equilibrium Fe-Mg fractionation, with increasing Fe (all ferrous) is: Tur < Bt < Krn < Spr < Grt. Krn appears in addition to Tur during the middle stage, because F, B, and water activities are buffered by the mineral assemblage and an anatectic melt. The absence of Krn is most granulite-facies pelitic gneisses, rocks that may have originally contained Tur, could be due to the absence of such buffering, resulting in loss of boron as Tur breaks down.

Research Organization:
Univ. of Maine, Orono (USA)
OSTI ID:
6596617
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English