Yamato 792947, 793408 and 82038: The most primitive H chondrites, with abundant refractory inclusions-Reference-Cited by-同舟云学术

Yamato 792947, 793408 and 82038: The most primitive H chondrites, with abundant refractory inclusions

Published:2002-10 Issue:10 Volume:37 Page:1417-1434
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:

Author:

Kimura M.,Hiyagon H.,Palme H.,Spettel B.,Wolf D.,Clayton R. N.,Mayeda T. K.,Sato T.,Suzuki A.,Kojima H.

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1945-5100.2002.tb01038.x/fullpdf

Reference48 articles.

1. Thermoluminescence sensitivity and thermal history of type 3 ordinary chondrites: Eleven new type 3.0-3.1 chondrites and possible explanations for differences among H, L, and LL chondrites;Benoit;Meteorit. Planet. Sci.,2002

2. Ca-Al-rich chondrules and inclusions in ordinary chondrites;Bischoff;Nature,1983

3. Al-rich objects in ordinary chondrites: Related origin of carbonaceous and ordinary chondrites and their constituents;Bischoff;Geochim. Cosmochim. Acta.,1984

4. Hammadah al Hamra 180: A unique unequilibrated chondrite with affinity to LL-group ordinary chondrites (abstract);Bischoff;Meteorit. Planet. Sci.,1997

5. Oxygen isotope studies of ordinary chondrites;Clayton;Geochim. Cosmochim. Acta.,1991

Cited by 28 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Calcium–aluminum‐rich inclusions in non‐carbonaceous chondrites: Abundances, sizes, and mineralogy;Meteoritics & Planetary Science;2023-05

2. Conditions of chondrule formation in ordinary chondrites;Geochimica et Cosmochimica Acta;2021-11

3. IIE irons: Origin, relationship to ordinary chondrites, and evidence for siderophile‐element fractionations caused by chondrule formation;Meteoritics & Planetary Science;2021-07-19

4. Petrology and classification of A‐9003, A 09535, and Y‐82094: A new type of carbonaceous chondrite;Meteoritics & Planetary Science;2021-07-12

5. Oxygen-isotope heterogeneity in the Northwest Africa 3358 (H3.1) refractory inclusions − Fluid-assisted isotopic exchange on the H-chondrite parent body;Geochimica et Cosmochimica Acta;2020-08