Decoupling of fluid and trace element release in subducting slab? Comment on "Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes" by C. Spandler et al. (Contrib Mineral Petrol 146:205-222, 2003)

Contributions to Mineralogy and Petrology

Volumn 148, Issue 4, 2004, Pages 502-505

  Liebscher, Axel ^a  

^a GeoForschungsZentrum Potsdam ^*  (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ECLOGITE; METAMORPHISM; SUBDUCTION ZONE; TRACE ELEMENT;

EID: 10444231994     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-004-0614-y     Document Type: Article

References (4)

1. Brunsmann A, Franz G, Erzinger J, Landwehr D (2000) Zoisite- and clinozoisite-segregations in metabasites (Tauern Window, Austria) as evidence for high-pressure fluid-rock interaction. J Metamorphic Geol 18:1-21 10.1046/j.1525-1314.2000.00233.x, 1:CAS:528:DC%2BD3cXivFGis7s%3D
2. Melzer S, Wunder B (2000) Island-arc basalt alkali ratios: Constraints from phengite-fluid partitioning experiments. Geology 28:583-586 10.1130/0091-7613(2000)028<0583:IABARC>2.3.CO;2, 1:CAS:528:DC%2BD3cXltVyjsrs%3D
3. Spandler C, Hermann J, Arculus R, Mavrognes J (2003) Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes. Contrib Mineral Petrol 146:205-222 10.1007/s00410-003-0495-5, 1:CAS:528:DC%2BD3sXovV2lur4%3D
4. Sun S-S, McDonough WF (1989) Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunders AD, Norry MJ (eds) Magmatism in the oceanic basins. Geol Soc Spec Publ 42:313-345