Front. Earth Sci.
Frontiers in Earth Science
Front. Earth Sci.
2296-6463
Frontiers Media S.A.
981906
10.3389/feart.2022.981906
Earth Science
Correction
Corrigendum: Qia’erdunbasixi Fe-Cu deposit in Sawur, Xinjiang: A case study of skarn deposit hosted by volcanic rock
Yang et al.
10.3389/feart.2022.981906
Yang
Shuang
1
Zhou
Qiu-Shi
1
Wang
Rui
1
*
Zhu
Yongfeng
2
*
1
State Key Laboratory of Geological Processes and Mineral Resources, and Institute of Earth Sciences, China University of Geosciences, Beijing, China
2
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Science, Peking University, Beijing, China
Edited and reviewed by: Hassan Mirnejad, Miami University, United States
*Correspondence: Rui Wang, rw@cugb.edu.cn; Yongfeng Zhu, yfzhu@pku.edu.cn
This article was submitted to Economic Geology, a section of the journal Frontiers in Earth Science
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Copyright © 2022 Yang, Zhou, Wang and Zhu.
2022
Yang, Zhou, Wang and Zhu
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
A Corrigendum on Qia’erdunbasixi Fe-Cu deposit in Sawur, Xinjiang: A case study of skarn deposit hosted by volcanic rock by Yang S, Zhou Q-S, Wang R and Zhu Y (2022). Front. Earth Sci. 10:852261. doi: 10.3389/feart.2022.852261
skarn
magnetite
syenite
Sawur
island arc
Fe-Cu deposit
In the published article, a citation of “Wang and Zhu, 2010” was erroneously missed. The citation has now been added in the caption of Figure 4. The updated caption can be seen below.
“FIGURE 4 | (A) Clinopyroxene is densely disseminated or presents as veinlets near the contact zone; (B) Magnetite is sparsely disseminated; (C) Magnetite veinlets; (D) Clinopyroxene is metasomatized by epidote + chlorite + magnetite, and epidotization and chloritization in the outer contact zone are well developed; (E–I) Alteration of quartz + magnetite + K-feldspar + calcite + sericite + chlorite + prehnite + actinolite + chalcopyrite + pyrite are developed in the hydrothermal stage; (F,G) Quartz-magnetite vein with a width of about 2∼10 cm, where magnetite accounts for as much as 40 vol.% of the vein volume; (J) Chalcopyrite is disseminated and magnetite is metasomatized by hematite; (K,L) Coarse K-feldspar grain, with inclusions of diopside formed in the early stage; (M) The calcite vein formed in the latest stage cuts through the early-stage magnetite; (N) Malachite in magnetite-quartz vein; (O) Wall rock of andesite is intensely mineralized with magnetite. Plane polarized light (A,E, M,O), cross polarized light (B–D,G–I,K,L,N), reflected light (J), BSE image (F). Ab—albite; Adr—andradite; Cal—calcite; Ccp—chalcopyrite; Chl—chlorite; Czo—clinozoisite; Di—diopside; Ep—epidote; Gl—glass; Hem—hematite; Mal—malachite; Mt—magnetite; Kfs—K-feldspar; Qtz—quartz; Sa—salite; Ser—sericite (modified after Wang and Zhu, 2010).”
The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
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