H Yurimoto, JT Wasson - 2002 - repository.geologyscience.ru
We describe a phenocryst in a CO-chondrite type-II chondrule that we infer to have formed by melting an amoeboid olivine aggregate (AOA). This magnesian olivine phenocryst has an …
H YURIMOTO, JT WASSON - Geochimica et Cosmochimica …, 2002 - ep.sci.hokudai.ac.jp
We describe a phenocryst in a CO-chondrite type-II chondrule that we infer to have formed by melting an amoeboid olivine aggregate (AOA). This magnesian olivine phenocryst has an …
H YURIMOTO - Geochimica et Cosmochimica Acta, 2002 - cir.nii.ac.jp
Extremely rapid cooling of a carbonaceous-chondrite chondrule containing very ^<16>O-rich olivine and a ^<26>Mg-excess | CiNii Research CiNii 国立情報学研究所 学術情報ナビゲータ[サイニィ …
H Yurimoto, JT Wasson - Geochimica et Cosmochimica Acta, 2002 - ui.adsabs.harvard.edu
We describe a phenocryst in a CO-chondrite type-II chondrule that we infer to have formed by melting an amoeboid olivine aggregate (AOA). This magnesian olivine phenocryst has an …
H Yurimoto, JT Wasson - Geochimica et Cosmochimica Acta, 2002 - infona.pl
We describe a phenocryst in a CO-chondrite type-II chondrule that we infer to have formed by melting an amoeboid olivine aggregate (AOA). This magnesian olivine phenocryst has an …
H Yurimoto, JT Wasson - Geochimica et Cosmochimica Acta, 2002 - cir.nii.ac.jp
Extremely rapid cooling of a carbonaceous-chondrite chondrule containing very 16O-rich olivine and a 26Mg-excess | CiNii Research CiNii 国立情報学研究所 学術情報ナビゲータ[サイニィ …
[引用][C]Extremely rapid cooling of a carbonaceous-chondrite chondrule containing very 16O-rich olivine and a 26Mg-excess
H YURIMOTO, JT WASSON - Geochimica et cosmochimica acta, 2002 - Elsevier