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Title: Nitrogen-isotope record of fluid-rock interactions in the Skiddaw Aureole and granite, English Lake District

Journal Article · · American Mineralogist
DOI:https://doi.org/10.2138/am-1999-1002· OSTI ID:20000951

The Skiddaw Granite and its contact metamorphic aureole in the English Lake District provide an excellent opportunity to test the capability of the N-isotope system to trace devolatilization and large-scale transfer of crustal fluids. In the aureole, Skiddaw Group metasedimentary rocks with relatively uniform lithology and major-element compositions show a dramatic decrease in N content toward the granite contact (from {ge}800 ppm at distances >2.5 km from the contact, to <410 ppm {le}0.55 km from the contact). Far from the intrusive body (>1.5 km), these rocks have extremely uniform {delta}{sup 15}N{sub air} near +3.7%, whereas closer to the contact ({le}1 km) {delta}{sup 15}N is shifted to higher values (up to +8.7%). The coupled decreases in N content and increases in {delta}{sup 15}N are compatible with the removal of N having low {delta}{sup 15}N in fluids during continuous, prograde devolatilization reactions involving the breakdown of white mica and the stabilization of biotite-, cordierite-, and andalusite-bearing assemblages. In the same metasedimentary rocks, the lack of obvious trends in major-element concentrations (including SiO{sub 2}/TiO{sub 2}, SiO{sub 2}/Al{sub 2}O{sub 3}, and the ratios of other major oxides to TiO{sub 2} and Al{sub 2}O{sub 3}) with distance from the granitic contact is consistent with minimal change in major element composition during the contact metamorphism. Ratios of whole-rock N, B, Rb, and Ba concentrations to whole-rock K{sub 2}O content are believed to reflect the differing fluid-mica partitioning (and involving varying relative proportions of white mica and biotite) of these trace elements during devolatilization reactions.

Research Organization:
Lehigh Univ., Bethlehem, PA (US)
OSTI ID:
20000951
Journal Information:
American Mineralogist, Vol. 84, Issue 10; Other Information: PBD: Oct 1999; ISSN 0003-004X
Country of Publication:
United States
Language:
English

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