Cumulates of arc magmas incorporated into the Sulu UHP metamorphic belt, eastern China

Abstract

Cumulates of arc magmas incorporated into the Sulu UHP metamorphic belt, eastern China Article no: 1101623 Enclosures:1) Query sheet 2) Article proofs Dear Author, 1. Please check these proofs carefully. It is the responsibility of the corresponding author to check these and approve or amend them. A second proof is not normally provided. Taylor & Francis cannot be held responsible for uncorrected errors, even if introduced during the production process. Once your corrections have been added to the article, it will be considered ready for publication.Please limit changes at this stage to the correction of errors. You should not make trivial changes, improve prose style, add new material, or delete existing material at this stage. You may be charged if your corrections are excessive (we would not expect corrections to exceed 30 changes).For detailed guidance on how to check your proofs, please paste this address into a new browser window: http://journalauthors.tandf.co.uk/production/checkingproofs.asp Your PDF proof file has been enabled so that you can comment on the proof directly using Adobe Acrobat. If you wish to do this, please save the file to your hard disk first. For further information on marking corrections using Acrobat, please paste this address into a new browser window: http://journalauthors.tandf.co.uk/production/acrobat.asp 2. Please review the table of contributors below and confirm that the first and last names are structured correctly and that the authors are listed in the correct order of contribution. This check is to ensure that your name will appear correctly online and when the article is indexed.

Petrogenesis of Early Carboniferous Ultramafic–Mafic Volcanic Rocks in the Southern Changning–Menglian Belt, Southeastern Tibetan Plateau: Implications for the Evolution of the Paleo‐Tethyan Ocean

“…6a). The clinopyroxene within the wehrlite has low Mg # values (79.4-85.6) and low concentrations of P 2 O 5 (<0.05 wt % ), suggesting that they are clinopyroxene megacrysts (Mg # < 85; P 2 O 5 ≤ 0.02 wt%) crystallized from the host lava (e.g., Hattori et al, 2010;Xie et al, 2016).…”