International audienceIntroduction: Large igneous inclusions are relatively rare and enigmatic components of ordinary chondrites, as they are only found in about 4% of this class of meteorites [1]. They can range up to several cm in diameter and are generally low in metal and sulfides. It has been suggested that individual large igneous inclusions could have formed by a range of mechanisms: some may have formed as unusually large chondrules [e.g. 1], others as impact melts [e.g. 1,2], igneous differentiates, or nebular melts formed at high-temperature via evaporation or condensation [e.g. 1,3]. Recently, O isotope analysis has demonstrated that some inclusions formed in distinct reservoirs before being incorporated into their host chondrite...
U-Th-Pb isotopic data are reported for mineral fractions, individual chondrules and fractions of cho...
International audienceThe IVA iron meteorites are magmatic cumulates from the core of a small astero...
We have performed instrumental and radiochemical neutron activation analyses of the host L6 chondrit...
International audienceIntroduction: Large igneous inclusions are relatively rare and enigmatic compo...
Large (>3.5 mm and up to 4 cm across) igneous inclusions poor in metal and sulfide are a minor but n...
Geochemical and isotopic data for large, igneous-textured inclusions in ordinary chondrites suggest ...
207Pb*/206Pb* chronometry was used to obtain the ages of Ca,Al-rich inclusions (CAIs) and chondrules...
Igneous inclusions and hosts of the Yamato ordinary chondrites Y-75097 (L6), Y-793241 (L6) and Y-794...
The Yamato-794046 H chondrite and its inclusion were dated by the Rb-Sr method as part of a consorti...
Our inventory of material from the early solar system includes large, igneous-textured inclusions in...
This thesis presents cosmochemical discoveries coupled with improvements of analytical techniques fo...
The impact histories on chondrite parent bodies can be deduced from thermochronologic analyses of ma...
We report on the mineralogy, petrography, and in situ oxygen isotopic composition of twenty-five ult...
Three ordinary chondrites from the Yamato Mountains (Y) region of Antarctica contain cm-sized igneou...
The 11th Symposium on Polar Science/Ordinary sessions: [OA] Antarctic meteorites, Thu. 3 Dec
U-Th-Pb isotopic data are reported for mineral fractions, individual chondrules and fractions of cho...
International audienceThe IVA iron meteorites are magmatic cumulates from the core of a small astero...
We have performed instrumental and radiochemical neutron activation analyses of the host L6 chondrit...
International audienceIntroduction: Large igneous inclusions are relatively rare and enigmatic compo...
Large (>3.5 mm and up to 4 cm across) igneous inclusions poor in metal and sulfide are a minor but n...
Geochemical and isotopic data for large, igneous-textured inclusions in ordinary chondrites suggest ...
207Pb*/206Pb* chronometry was used to obtain the ages of Ca,Al-rich inclusions (CAIs) and chondrules...
Igneous inclusions and hosts of the Yamato ordinary chondrites Y-75097 (L6), Y-793241 (L6) and Y-794...
The Yamato-794046 H chondrite and its inclusion were dated by the Rb-Sr method as part of a consorti...
Our inventory of material from the early solar system includes large, igneous-textured inclusions in...
This thesis presents cosmochemical discoveries coupled with improvements of analytical techniques fo...
The impact histories on chondrite parent bodies can be deduced from thermochronologic analyses of ma...
We report on the mineralogy, petrography, and in situ oxygen isotopic composition of twenty-five ult...
Three ordinary chondrites from the Yamato Mountains (Y) region of Antarctica contain cm-sized igneou...
The 11th Symposium on Polar Science/Ordinary sessions: [OA] Antarctic meteorites, Thu. 3 Dec
U-Th-Pb isotopic data are reported for mineral fractions, individual chondrules and fractions of cho...
International audienceThe IVA iron meteorites are magmatic cumulates from the core of a small astero...
We have performed instrumental and radiochemical neutron activation analyses of the host L6 chondrit...