文献
J-GLOBAL ID:201502207377529882
整理番号:15A0110151
チベット,Luobusaオフィオライトのポディフォーム型クロム鉄鉱岩とそれに伴うマントルかんらん岩中の超高圧で高度に還元された鉱物の起源
Origin of ultrahigh pressure and highly reduced minerals in podiform chromitites and associated mantle peridotites of the Luobusa ophiolite, Tibet
著者 (6件):
XU Xiangzhen
(State Key Lab. of Continental Tectonic and Dynamics, Inst. of Geology, Chinese Acad. of Geological Sciences, Beijing ...)
,
YANG Jingsui
(State Key Lab. of Continental Tectonic and Dynamics, Inst. of Geology, Chinese Acad. of Geological Sciences, Beijing ...)
,
ROBINSON Paul T.
(State Key Lab. of Continental Tectonic and Dynamics, Inst. of Geology, Chinese Acad. of Geological Sciences, Beijing ...)
,
XIONG Fahui
(State Key Lab. of Continental Tectonic and Dynamics, Inst. of Geology, Chinese Acad. of Geological Sciences, Beijing ...)
,
BA Dengzhu
(State Key Lab. of Continental Tectonic and Dynamics, Inst. of Geology, Chinese Acad. of Geological Sciences, Beijing ...)
,
GUO Guolin
(State Key Lab. Breeding Base of Nuclear Resources and Environment, East China Inst. of Technol., Nanchang 330013, CHN)
資料名:
Gondwana Research
(Gondwana Research)
巻:
27
号:
2
ページ:
686-700
発行年:
2015年02月
JST資料番号:
W2249A
ISSN:
1342-937X
資料種別:
逐次刊行物 (A)
記事区分:
原著論文
発行国:
オランダ (NLD)
言語:
英語 (EN)