Assessing the utility of thallium and thallium isotopes for tracing subduction zone inputs to the Mariana arc

Chemical Geology

Volumn 345, Issue , 2013, Pages 139-149

  Prytulak, J ^a,b   Nielsen, S G ^a,c   Plank, T ^d   Barker, M ^a,e   Elliott, T ^f  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b IMPERIAL COLLEGE LONDON   (United Kingdom)

^c WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^d International Research Institute for Climate and Society   (United States)

^e ATKINS   (United Kingdom)

^f UNIVERSITY OF BRISTOL   (United Kingdom)

Author keywords

Mariana Islands; Phengite; Subduction; Thallium stable isotopes

Indexed keywords

ALTERED OCEANIC CRUSTS; ISOTOPE COMPOSITIONS; MARIANA ISLANDS; ORDERS OF MAGNITUDE; PHENGITE; STABLE ISOTOPES; SUBDUCTION; THERMAL PARAMETERS;

LEAD; MICA; SEDIMENTOLOGY; SEDIMENTS; TECTONICS; THALLIUM;

ISOTOPES;

CONCENTRATION (COMPOSITION); ISOTOPIC COMPOSITION; LAVA; MARINE SEDIMENT; OCEANIC CRUST; PHENGITE; STABLE ISOTOPE; SUBDUCTION ZONE; THALLIUM; TRACER;

MARIANA ARC; MARIANA ISLANDS; PACIFIC OCEAN;

MICAS;

EID: 84876325532     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2013.03.003     Document Type: Article

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