Chlorine isotope behavior in subduction zone settings revealed by olivine-hosted melt inclusions from the Central America Volcanic Arc

Bouvier A.-S, Portnyagin MV, Flemetakis S, Hoernle K, Klemme S, Berndt J, Mironov N, John T

Research article (journal)

Abstract

The isotopic composition of Cl, a highly hydrophilic and incompatible element, can provide new insights into the processes of element recycling in subduction zone settings. Samples from 13 localities in Guatemala, El Salvador, Nicaragua and Costa Rica, representing a ca. 1000 km long NW-SE segment along the Central American Volcanic Arc (CAVA), were selected. Ninety-seven melt inclusions, hosted by olivine Fo90-70, were measured for Cl isotope ratios and trace element concentrations. Melt inclusions from samples from Guatemala to northwest Nicaragua have a restricted range of d37Cl values (range < 1‰ within a sample) with values decreasing from Santa Maria (Guatemala) to San Miguel (El Salvador), whereas melt inclusions from Nicaragua and Costa Rica display larger variation within a sample (d37Cl value range >1‰, up to 3.8‰) and do not show any systematic variation along the arc. For some samples, the d37Cl in the melt inclusions is shifted by up to 2‰ to higher values compared to bulk rock data from the same volcanic center, for which the extent of Cl degassing is not known. The combination of d37Cl values in melt inclusions with trace elements and the existing knowledge about the slab contributions along the arc allows us to elucidate the Cl isotope composition of different endmembers in this subduction zone. From Guatemala to northwest Nicaragua, a fluid component, originating from serpentinite, has a d37Cl value close to +0.6‰. This value, similar to lithospheric serpentinites, confirms that despite the aqueous fluid migration through the entire slab, Cl isotopes do not fractionate significantly during transport. A melt-like component, present in the southern part of the arc, has d37Cl of -0.8‰ (possibly down to -2.5‰). This signature is lower than d37Cl values of the oceanic crust but similar to sediments currently subducting beneath CAVA. Finally, a common component, most likely amphibole-bearing metasomatized mantle, is identified in samples with the highest d37Cl values (up to +3.0‰). The melting of amphibole, mineral concentrating 37Cl over 35Cl, could explain the high d37Cl values. The difference between melt inclusions and bulk rock d37Cl in some volcanic centers probably results from late stage processes such as assimilation of magmatic brine or mixing of different batches of magma at shallower levels after melt inclusions entrapment: melts with strong signature (high d37Cl) from the metasomatized (amphibole-bearing) mantle will be diluted by melts with the signature of the two other endmembers, which have lower d37Cl and similar or higher Cl contents. Melt inclusions thus give a more precise picture of Cl isotope systematics in primitive subduction-related magmas.

Details zur Publikation

Release year: 2022
Language in which the publication is written: English