Journal Title
Title of Journal: Contrib Mineral Petrol
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Abbravation: Contributions to Mineralogy and Petrology
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Publisher
Springer Berlin Heidelberg
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Authors: A Didier V Bosse J Bouloton S Mostefaoui M Viala J L Paquette J L Devidal R Duhamel
Publish Date: 2015/10/31
Volume: 170, Issue: 5-6, Pages: 45-
Abstract
In this study we use NanoSIMS element and isotope ratio mapping and LAICPMS trace element measurements to elucidate the origins of monazites from a restitic xenolith enclosed in a 135 ± 03 Ma andesitic lava Slovakia The xenolith/lava interaction is mainly characterized by the growth of a plagioclasebearing corona around the xenolith and magmatic garnet overgrowths on primary metamorphic garnets within the xenolith NanoSIMS images 89Y 139La 208Pb 232Th and 238U and trace element analyses indicate that variations of HREE Y and Eu contents in the monazite are correlated with the resorption and the following overgrowth of garnet and plagioclase in the xenolith Three domains are distinguished in the monazite grains the inherited Variscan core at ca 310 Ma M1 domain characterized by low Y and HREE contents and a weak negative Eu anomaly the inner rim M2 domain crystallized during the growth of the plagioclase magmatic corona large negative Eu anomaly and the resorption of metamorphic garnet high HREE and Y contents and the external rim M3 domain crystallized during the growth of the plagioclase corona large negative Eu anomaly and during the crystallization of magmatic garnet low Y HREE contents at ~13 Ma ie the age of the andesitic lava The age and chemical zonation of the monazites attest to the preservation of primary monazite in the xenolith despite the interaction with the andesite lava NanoSIMS imaging provides highquality subµm scale images of the monazite that reveals chemical domains that were not distinguishable on WDS Xray maps especially for depleted elements such as U and Pb Owing to its small size the M2 domain could not be accurately dated by the LAICPMS method However NanoSIMS isotopic maps reveal that the M2 domain has similar 208Pb/232Th isotope ratios to the M3 domain and thus similar ages These results support the hypothesis that meltassisted partial dissolution–precipitation in monazite efficiently records chemical and mineralogical changes during xenolith/lava interactionThanks are due to JeanMarc Hénot for his help in the use of SEM Emily Mullen for English corrections and O Laurent for fruitful discussion The paper has been greatly improved by the critical and constructive comments of Alexander Stepanov and an anonymous reviewer This work is supported a posteriori by CNRSINSU
Keywords:
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Other Papers In This Journal:
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- Formation of cordierite-bearing lavas during anatexis in the lower crust beneath Lipari Island (Aeolian arc, Italy)
- An Early Cretaceous garnet pressure–temperature path recording synconvergent burial and exhumation from the hinterland of the Sevier orogenic belt, Albion Mountains, Idaho
- Crystal reaming during the assembly, maturation, and waning of an eleven-million-year crustal magma cycle: thermobarometry of the Aucanquilcha Volcanic Cluster
- Origin of phlogopite-orthopyroxene inclusions in chromites from the Merensky Reef of the Bushveld Complex, South Africa
- An empirical garnet (YAG) – xenotime thermometer
- Magma storage and mixing conditions for the 1953–1974 eruptions of Southwest Trident volcano, Katmai National Park, Alaska
- In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites
- Reply to comments by Sengupta, Raith and Dasgupta on S. B. Bhattacharya and R. K. Kar (2002)
- Trace element mapping by LA-ICP-MS: assessing geochemical mobility in garnet
- Metasomatized lithospheric mantle beneath Turkana depression in southern Ethiopia (the East Africa Rift): geochemical and Sr–Nd–Pb isotopic characteristics
- In situ observations of bubble growth in basaltic, andesitic and rhyodacitic melts
- Phosphorus-controlled trace element distribution in zircon revealed by NanoSIMS
- Hydroxyl in olivines from mantle xenoliths in kimberlites of the Siberian platform
- Electrical conductivity of orthopyroxene and plagioclase in the lower crust
- Chromite in komatiites: 3D morphologies with implications for crystallization mechanisms
- In situ Sr isotopic analyses of epidote: tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite (Ganghe, Dabie terrane)
- Source components of the Gran Canaria (Canary Islands) shield stage magmas: evidence from olivine composition and Sr–Nd–Pb isotopes
- The stability and origin of sodicgedrite in ultrahigh-temperature Mg-Al granulites: a case study from the Gondwana suture in southern India
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- The Campanian Ignimbrite (southern Italy) geochemical zoning: insight on the generation of a super-eruption from catastrophic differentiation and fast withdrawal
- Melting of clinopyroxene + magnesite in iron-bearing planetary mantles and implications for the Earth and Mars
- Immiscible separation of metalliferous Fe/ Ti-oxide melts from fractionating alkali basalt: P - T - f O2 conditions and two-liquid elemental partitioning
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- A case for hornblende dominated fractionation of arc magmas: the Chelan Complex (Washington Cascades)
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- Shoshonite and sub-alkaline magmas from an ultrapotassic volcano: Sr–Nd–Pb isotope data on the Roccamonfina volcanic rocks, Roman Magmatic Province, Southern Italy
- The role of slab melting in the petrogenesis of high-Mg andesites: evidence from Simbo Volcano, Solomon Islands
- Evolution of the Taupo Volcanic Center, New Zealand: petrological and thermal constraints from the Omega dacite
- Multi-stage metasomatism of diamondiferous eclogite xenoliths from the Udachnaya kimberlite pipe, Yakutia, Siberia
- Hercynian, Pan-African, Proterozoic and Archean ion-microprobe zircon ages for a Betic-Rif core complex, Alpine belt, W Mediterranean – consequences for its P - T - t path
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