Recycling and transport of continental material through the mantle wedge above subduction zones: a Caribbean example

Rojas-Agramonte, Yamirka, Garcia-Casco, Antonio, Kemp, Anthony, Kröner, Alfred, Proenza, Joaquín A., Lázaro, Concepción, and Liu, Dunyi (2016) Recycling and transport of continental material through the mantle wedge above subduction zones: a Caribbean example. Earth and Planetary Science Letters, 436. pp. 93-107.

[img] PDF (Published Version) - Published Version
Restricted to Repository staff only

View at Publisher Website:


Estimates of global growth rates of continental crust critically depend upon knowledge of the rate at which crustal material is delivered back into the mantle at subduction zones and is then returned to the crust as a component of mantle-derived magma. Quantification of crustal recycling by subduction-related magmatism relies on indirect chemical and isotopic tracers and is hindered by the large range of potential melt sources (e.g., subducted oceanic crust and overlying chemical and clastic sediment, sub-arc lithospheric mantle, arc crust), whose composition may not be accurately known. There is also uncertainty about how crustal material is transferred from subducted lithosphere and mixed into the mantle source of arc magmas. We use the resilient mineral zircon to track crustal recycling in mantle-derived rocks of the Caribbean (Greater Antilles) intra-oceanic arc of Cuba, whose inception was triggered after the break-up of Pangea. Despite juvenile Sr and Nd isotope compositions, the supra-subduction zone ophiolitic and volcanic arc rocks of this Cretaceous (similar to 135-70 Ma) arc contain old zircons (similar to 200-2525 Ma) attesting to diverse crustal inputs. The Hf-O isotope systematics of these zircons suggest derivation from exposed crustal terranes in northern Central America (e.g. Mexico) and South America. Modeling of the sedimentary component in the most mafic lavas suggests a contribution of no more than 2% for the case of source contamination or less than 4% for sediment assimilation by the magma. We discuss several possibilities for the presence of inherited zircons and conclude that they were transported as detrital grains into the mantle beneath the Caribbean Plate via subduction of oceanic crust. The detrital zircons were subsequently entrained by mafic melts that were rapidly emplaced into the Caribbean volcanic arc crust and supra-subduction mantle. These findings suggest transport of continental detritus, through the mantle wedge above subduction zones, in magmas that otherwise do not show strong evidence for crustal input and imply that crustal recycling rates in some arcs may be higher than hitherto realized.

Item ID: 43231
Item Type: Article (Research - C1)
ISSN: 1385-013X
Keywords: crustal recycling, zircon U-Pb geochronology, inherited zircon, Hf isotopes, O isotopes, Cuba
Funders: Deutsche Forschungsgemeinschaft (DFG), MINECO, Secretariat for Higher Education, Science, Technology and Innovation, Ecuador
Projects and Grants: DFG KR590/85-1 & RO4174/2-1, MINECO CGL2013-40785-P & CGL2012-36263, Synthesys Programme GB-TAF-4245
Date Deposited: 09 Mar 2016 07:31
FoR Codes: 37 EARTH SCIENCES > 3705 Geology > 370511 Structural geology and tectonics @ 50%
37 EARTH SCIENCES > 3705 Geology > 370509 Sedimentology @ 50%
SEO Codes: 97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%
Downloads: Total: 1
More Statistics

Actions (Repository Staff Only)

Item Control Page Item Control Page