A vacancy-rich, partially inverted spinelloid silicate, (Mg,Fe,Si)(2)(Si,)O-4, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites

doi:10.1111/maps.13349

	Ma, Chi 1; Tschauner, Oliver 2; Bindi, Luca 3,4; Beckett, John R.1; Xie, Xiande 5,6
	A vacancy-rich, partially inverted spinelloid silicate, (Mg,Fe,Si)(2)(Si,)O-4, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites
Source Publication	METEORITICS & PLANETARY SCIENCE
ISSN	1086-9379
	2019-09-01
Volume	54 Issue:9 Pages:1907-1918
DOI	10.1111/maps.13349
Language	英语
WOS Research Area	Geochemistry & Geophysics
WOS ID	WOS:000486197300002
Indexed By	SCI
Citation statistics	Cited Times:12[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/47137
Collection	中国科学院矿物学与成矿学重点实验室
Corresponding Author	Ma, Chi
Affiliation	1.CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA 2.Univ Nevada, Dept Geosci, Las Vegas, NV 89154 USA 3.Univ Firenze, Dipartimento Sci Terra, Via G La Pira 4, I-50121 Florence, Italy 4.CNR, Ist Geosci & Georisorse, Sez Firenze, Via G La Pira 4, I-50121 Florence, Italy 5.Chinese Acad Sci, Key Lab Mineral & Metallogeny, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China 6.Chinese Acad Sci, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou 510640, Guangdong, Peoples R China
Recommended Citation GB/T 7714	Ma, Chi,Tschauner, Oliver,Bindi, Luca,et al. A vacancy-rich, partially inverted spinelloid silicate, (Mg,Fe,Si)(2)(Si,)O-4, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites[J]. METEORITICS & PLANETARY SCIENCE,2019,54(9):1907-1918.
APA	Ma, Chi,Tschauner, Oliver,Bindi, Luca,Beckett, John R.,&Xie, Xiande.(2019).A vacancy-rich, partially inverted spinelloid silicate, (Mg,Fe,Si)(2)(Si,)O-4, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites.METEORITICS & PLANETARY SCIENCE,54(9),1907-1918.
MLA	Ma, Chi,et al."A vacancy-rich, partially inverted spinelloid silicate, (Mg,Fe,Si)(2)(Si,)O-4, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondrites".METEORITICS & PLANETARY SCIENCE 54.9(2019):1907-1918.

Files in This Item:
There are no files associated with this item.

If you have any objections to this item, please fill out the form below and the administrator will contact you as soon as possible.
Content:
Email：	*
Institution:
Verification Code:	Refresh

Any comments and suggestions are welcomed.
Title:	*
Content:
Email：	*
Verification Code:	Refresh

中国科学院广州地球化学研究所机构知识库