Satish-Kumar, MHermann, JoergMiyamoto, TOsanai, Y2015-12-100024-4937http://hdl.handle.net/1885/55867Granulite grade marble layers interlayered with metapelitic granulites from Lützow Holm Bay, East Antarctica, provide insight into fluid-rock interactions during burial to and exhumation from lower crustal levels. Sub-millimeter scale strontium, oxygen aKeywords: burial (geology); carbon isotope; exhumation; fluid inclusion; geochemistry; heterogeneity; inductively coupled plasma method; infiltration; isotopic composition; marble; metasomatism; overprinting; oxygen isotope; rare earth element; recrystallization; r East Antarctica; Fluid infiltration; Marbles; O and C isotopes; REE chemistry; SrFingerprinting a multistage metamorphic fluid-rock history: Evidence from grain scale Sr, O and C isotopic and trace element variations in high-grade marbles from East Antarctica201010.1016/j.lithos.2009.08.0102016-02-24