Results 121 to 130 of about 45,209 (160)
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Meteoritics & Planetary Science, 2023
Cosmochemists have relied on CI carbonaceous chondrites as proxies for chemical composition of the non‐volatile elements in the solar system because these meteorites are fine‐grained, chemically homogeneous, and have well‐determined bulk compositions ...
David R. Frank +4 more
semanticscholar +1 more source
Cosmochemists have relied on CI carbonaceous chondrites as proxies for chemical composition of the non‐volatile elements in the solar system because these meteorites are fine‐grained, chemically homogeneous, and have well‐determined bulk compositions ...
David R. Frank +4 more
semanticscholar +1 more source
Infall and Disk Processes – the Message from Meteorites
Space Science ReviewsHow do planetary systems, in general, and our own Solar System (SS), in particular, form? In conjunction, Astronomy and Isotope Cosmochemistry provide us with powerful tools to answer this age-old question. In this contribution, we review recent advances
F. L. Tissot +7 more
semanticscholar +1 more source
Volume measurement of microparticles using SEM photogrammetry and 3‐D reconstruction
Meteoritics & Planetary ScienceIn this paper, we introduce a method for volume measurement of microparticles that includes scanning electron microscope photogrammetry with 3‐D model construction.
Y. Zheng +4 more
semanticscholar +1 more source
Highly siderophile element nano‐nuggets in Wabar impact glass
Meteoritics & Planetary ScienceCirca 300 years ago, a ~15‐m iron asteroid impacted sand dunes in the Empty Quarter of Saudi Arabia, creating the Wabar craters and fragments of the IIIAB Wabar iron meteorite. A significant portion of the asteroid dissolved into the sand, forming a wide
Axel Wittmann, Marc Biren
semanticscholar +1 more source
Meteoritics & Planetary Science
Abundances, apparent sizes, and individual chemical compositions of chondrules, refractory inclusions, other objects, and surrounding matrix have been determined for Semarkona (LL3.00) and Renazzo (CR2) using consistent methods and criteria on X‐ray ...
Denton S. Ebel +5 more
semanticscholar +1 more source
Abundances, apparent sizes, and individual chemical compositions of chondrules, refractory inclusions, other objects, and surrounding matrix have been determined for Semarkona (LL3.00) and Renazzo (CR2) using consistent methods and criteria on X‐ray ...
Denton S. Ebel +5 more
semanticscholar +1 more source
Metal–forsterite condensate nodules and H‐L‐LL compositions
Meteoritics & Planetary ScienceCompared to the carbonaceous chondrites (CCs), ordinary chondrites (OCs) are depleted in Mg and refractory lithophile elements. The OCs are classified by a trend from high metal (H) to low total iron (L) to low total iron and low metal (LL) compositions ...
Denton S. Ebel +3 more
semanticscholar +1 more source
Corundum ± magnesium‐deltalumite ± hibonite‐bearing objects in the CH chondrite Sayh al Uhaymir 290
Meteoritics & Planetary ScienceIsolated corundum grains and corundum ± Mg‐deltalumite [(Al,Mg)(Al,◻)2O4] ± hibonite assemblages were investigated in the CH3.0 metal‐rich carbonaceous chondrite Sayh al Uhaymir (SaU) 290.
Konstantin M. Ryazantsev +5 more
semanticscholar +1 more source
Meteoritics & Planetary Science
Calcium–aluminum‐rich inclusions (CAIs) in chondrites are one of the oldest materials in the solar system. Presence of refractory minerals in CAIs suggests that they formed thorough a condensation process from nebular gas of solar composition.
Y. Masuda +3 more
semanticscholar +1 more source
Calcium–aluminum‐rich inclusions (CAIs) in chondrites are one of the oldest materials in the solar system. Presence of refractory minerals in CAIs suggests that they formed thorough a condensation process from nebular gas of solar composition.
Y. Masuda +3 more
semanticscholar +1 more source
Meteoritics & Planetary Science
Camel Donga 003 (CD 003) was originally classified as a CK3 chondrite based on its coarse‐grained matrix, Ni‐rich sulfides, Cr‐rich magnetite, and CK‐like silicate mineralogy.
E. G. Alevy +4 more
semanticscholar +1 more source
Camel Donga 003 (CD 003) was originally classified as a CK3 chondrite based on its coarse‐grained matrix, Ni‐rich sulfides, Cr‐rich magnetite, and CK‐like silicate mineralogy.
E. G. Alevy +4 more
semanticscholar +1 more source

