Search results for " refertilization."

showing 2 items of 2 documents

The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths

2021

We present the first isotopic (noble gases and CO2) characterization of fluid inclusions coupled to Raman microspectroscopy analyses in mantle xenoliths from Central Mexico, a geodynamically complex area where the Basin and Range extension was superimposed on the Farallon subduction (terminated at 28 Ma). To characterize the isotopic signature of the Central Mexican lithospheric mantle, we focus on fluid inclusions entrapped in mantle xenoliths found in deposits of the Joya Honda maar (JH), a Quaternary monogenetic volcano belonging to the Ventura Espiritu Santo Volcanic Field (VESVF) in the state of San Luis Potosí (central Mexico). Thirteen ultramafic plagioclase-free xenoliths were selec…

GEO/07 - PETROLOGIA E PETROGRAFIA010504 meteorology & atmospheric sciencesCarbonate recyclingGeochemistry2010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundNoble gaseGeochemistry and PetrologyUltramafic rockGEO/08 - GEOCHIMICA E VULCANOLOGIAXenolithFluid inclusionsMetasomatismFarallon Plate0105 earth and related environmental sciencesMantle refertilizationSubductionGeologyFluid inclusionSilicateCOchemistryCarbonate recycling CO2 Fluid inclusions Mantle refertilization Mexican mantle xenoliths Noble gasesGeologyMexican mantle xenolith
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Noble gas and CO2 isotopic signatures of the lithospheric mantle underneath Mexico and the Canary Islands: clues from mantle xenoliths and arc lavas

2022

Studying the isotopic composition of fluids trapped in mantle xenoliths opens avenues to understand the origin and cycling of volatiles in the Earth’s upper mantle. In this PhD dissertation, new and in most cases the very first data regarding the isotopic (noble gases and CO2) characterization of the lithospheric mantle portions of three different geodynamic environments are presented: (i) Central and NW Mexico, a continental setting dominated by extension; (ii) the Transmexican Volcanic Belt (TMVB) a subduction setting, and (iii) the Canary Islands, particularly El Hierro and Lanzarote, two oceanic islands formed by mantle plume-derived intraplate volcanism. In total 32 peridotites (includ…

Mexico Canary Islands lithospheric mantle subduction mantle plume continental rift Basin and Range volcanism mantle xenoliths fluid inclusions noble gas isotopes carbon isotopes carbon recycling refertilization.Settore GEO/08 - Geochimica E Vulcanologia
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