1. Primary Sulfur Isotopes of Intraplate Basalts and Implications for Deep S Recycling of Altered Oceanic Crust.
- Author
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Wang, Xiang, Wang, Zaicong, Sun, Pu, Yang, Zong‐Feng, Zhang, Wen, Zou, Zongqi, Foley, Stephen, Wang, Lang, Zong, Keqing, Hu, Zhaochu, and Liu, Yongsheng
- Subjects
SLABS (Structural geology) ,SULFUR isotopes ,OCEANIC crust ,SULFUR cycle ,PERIDOTITE ,SUBDUCTION zones ,SUBDUCTION ,ORE deposits - Abstract
Altered oceanic crust (AOC) is the largest contributor to the subducted sulfur (S) budget and its recycling modulates the redox evolution and S distribution in the mantle. However, the role of AOC in the deep cycling of S remains poorly constrained. Here we probe the primary S isotopes of Cenozoic intraplate basalts in eastern China by investigating sulfide inclusions in magmatic clinopyroxene megacrysts. These basalts were derived from the deep mantle metasomatized by melts derived from recycled AOC but show MORB‐like S isotopes (−0.9–0.9‰), suggesting that AOC‐derived melts transfer negligible sulfate and hardly change the δ34S and redox state of the deeper mantle. This contrasts with the generally high δ34S values of mantle wedge peridotites and primary arc magmas that reflect the slab addition of sulfate, indicating that S species and isotopes released from the subducted slab and associated fO2 are not constant and vary with subduction depth. Plain Language Summary: Subduction‐driven recycling of S plays a key role in the redox evolution of the mantle, the formation of ore deposits, and climatic impact through volcanic emission of SO2. Altered oceanic crust (AOC) is the largest contributor to the subducted S budget but the role of AOC in the deep cycling of S remains poorly constrained. Here we present high‐precision in‐situ S isotopes of sulfide inclusions in magmatic clinopyroxene megacrysts captured by Cenozoic intraplate basalts in eastern China, which were sourced from the deep mantle affected by melts derived from recycled AOC within the Pacific slab. The sulfide inclusions are not affected by magmatic differentiation or degassing and reveal the primary δ34S of intraplate basalts and their mantle sources. The mid‐ocean ridge basalts (MORB)‐like δ34S values in deep mantle sources indicate that AOC‐derived melts are mainly sulfide‐saturated and could not modify the δ34S and redox state of the deep mantle significantly. This is in contrast to the high δ34S values of mantle wedge peridotites and primary arc magmas that require the addition of sulfate from the slab or sulfur disproportionation at sub‐arc depth, suggesting that S species and isotopic composition of materials released from the subducted slab vary with subduction depth. Key Points: Sulfur isotopes of sulfide inclusions in clinopyroxene megacrysts reveal the primary δ34S of intraplate basaltsDeeply subducted oceanic crust hardly changes the δ34S and redox state of the mantleSulfur species and isotopes released from the subducted oceanic slab and associated fO2 are not constant and vary with subduction depth [ABSTRACT FROM AUTHOR]
- Published
- 2024
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