Al–Mg isotope records in sixteen ferromagnesian chondrules from five unequilibrated
ordinary chondrites (UOCs), four L chondrites with petrologic grades varying from 3.0 to 3.2 …

We performed a systematic high‐precision secondary ion mass spectrometry 26Al‐26Mg
isotopic study for 11 ferromagnesian chondrules from the highly unequilibrated ordinary …

We have conducted systematic investigations of formation age, chemical compositions, and
mineralogical characteristics of ferromagnesian chondrules in Yamato-81020 (CO3. 05) …

Fossil records of the now-extinct short-lived nuclide 26Al were analyzed in twelve
chondrules from four unequilibrated ordinary chondrites (UOCs), Semarkona (3.0) …

We have studied the relationship between bulk chemical compositions and relative
formation ages inferred from the initial 26Al/27Al ratios for sixteen ferromagnesian …

Chondrules in ordinary chondrites are considered to form in high density environments,
likely related to the evolution of protoplanets and large planetesimals. In order to determine …

The 26Al–26Mg systems of five ferromagnesian chondrules from the least metamorphosed
ordinary chondrite Semarkona (LL3. 0) were studied using a secondary ion mass …

Deciphering the spatial and temporal evolution of chondrules allows for a better
understanding of how asteroidal seeds formed, migrated, and eventually accreted into …

Abstract 26 Al-26 Mg ages were determined for 14 anorthite-bearing chondrules from five
different unequilibrated ordinary chondrites (UOCs) with low petrologic subtypes (3.00 …

Chondrules are high-temperature components of meteorites and are formed during flash
heating episodes in the early solar system. From the presence of compound chondrules …