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))

Abstract

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.