T Kleine, K Mezger, H Palme, E Scherer… - … et Cosmochimica Acta, 2005 - Elsevier
The 182Hf-182W isotopic systematics of Ca-Al-rich inclusions (CAIs), metal-rich chondrites, and iron meteorites were investigated to constrain the relative timing of accretion of their …
In ordinary chondrites (OCs), feldspar is present both in chondrules as a primary, igneous phase, and as a secondary phase that results from crystallization of chondrule mesostasis …
K Kehm, EH Hauri, CMOD Alexander… - … et Cosmochimica Acta, 2003 - Elsevier
The first cold plasma ICP-MS (inductively coupled plasma mass spectrometer) Fe isotope study is described. Application of this technique to the analyses of Fe isotopes in a number …
G Libourel, AN Krot - Earth and Planetary Science Letters, 2007 - Elsevier
Chondrules are the major high-temperature components of chondritic meteorites, which are conventionally viewed as the samples from the very first generation of undifferentiated …
Chondrites are the largest group of meteorites. They can provide unique insights into the origins and early evolution of our Solar System, and even into the relationships between our …
SS Russell, M Gounelle… - … Transactions of the …, 2001 - royalsocietypublishing.org
This paper reviews the evidence for short–lived radionuclides in the early Solar System and critically evaluates models for their origin. Radionuclides with half–lives of less than 50 Myr …
TD Swindle - Reviews in mineralogy and geochemistry, 2002 - pubs.geoscienceworld.org
One of the reasons noble gases make such good tracers of processes occurring in rocks is their scarcity. Thus, a process that converts a small fraction of a relatively rare element into a …
The recently recovered paired Antarctic achondrites Graves Nunatak 06128 and 06129 (GRA) are meteorites that represent unique high-temperature asteroidal processes that are …
We summarize geochemical, astronomical, and theoretical constraints on the lifetime of the protoplanetary disk. Absolute Pb-Pb-isotopic dating of CAIS in CV chondrites (4567.2±0.7 …