气候变化领域集成服务门户(CCPortal): Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))

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DOI	10.1016/j.epsl.2020.116136
	Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))
	Xiong Q.; Xu Y.; González-Jiménez J.M.; Liu J.; Alard O.; Zheng J.-P.; Griffin W.L.; O'Reilly S.Y.
发表日期	2020
ISSN	0012821X
卷号	535
英文摘要	The authors regret two errors within the Oman dunite samples, these should be corrected as follows: [1] Two dunites from the Wadi Tayin massif of the SE Oman ophiolite should be listed as from the dunite channel system within the upper mantle, not from the Moho transition zone. (1) Two sentences in the last paragraph of Section 1 (Introduction, page 1) should read as: Rhenium-Os isotopes of dunites from the Moho transition zone and mantle depths of the Samail (or called Sumail) and Wadi Tayin massifs in the Oman ophiolite were analyzed by N-TIMS for comparison. Whole-rock major- and trace-element compositions of the Zedang dunites are also reported here.(2) The first sentence of the second paragraph of Section 2.2 (page 4) should read as: The dunites from the Oman ophiolite were collected from the Moho transition zone in the Samail massif (3 samples) and from the mantle depths in the Wadi Tayin massif (2 samples).[2] The sample location, whole-rock major and trace element compositions (Table A2 and Fig. A4 in our paper) of the five Oman dunites have been published by Godard et al. (2000) [Godard, M., Jousselin, D., Bodinier, J.-L., 2000. Relationships between geochemistry and structure beneath a palaeo-spreading centre: a study of the mantle section in the Oman ophiolite. Earth Planet. Sci. Lett. 180, 133–148]. In addition, the method description (the last three sentences of Section 3.2, page 4) of these Oman samples should be deleted. [3] Table A2 is updated in the Supplementary Material. The authors appreciate that Dr. Marguerite Godard kindly reminded us these errors and gave comments on this corrigendum. We apologize for these errors and any inconvenience that this might cause. © 2020 Elsevier B.V.
语种	英语
来源期刊	Earth and Planetary Science Letters
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/202973
作者单位	State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), GEMOC, Department of Earth and Planetary Sciences, Macquarie UniversityNSW 2109, Australia; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, China; Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Avda. Fuentenueva s/n, Granada, 18002, Spain; Geosciences Montpellier, CNRS UMR5243, Université de Montpellier, Pl. E. Bataillon, Montpellier, 34095, France
推荐引用方式 GB/T 7714	Xiong Q.,Xu Y.,González-Jiménez J.M.,等. Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))[J],2020,535.
APA	Xiong Q..,Xu Y..,González-Jiménez J.M..,Liu J..,Alard O..,...&O'Reilly S.Y..(2020).Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969)).Earth and Planetary Science Letters,535.
MLA	Xiong Q.,et al."Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))".Earth and Planetary Science Letters 535(2020).