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Petrogenesis of volcanic rocks from Eastern Manus Basin: indications in mineralogy and geochemistry

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Abstract

To understand the petrogenesis and magma evolution history in the Eastern Manus Basin (EMB), geochemistry of pyroxene and plagioclase mineral phenocrysts in basaltic andesites and dacites were reported. The plagioclase-melt thermometry showed that, plagioclase in dacites crystalized in 1 027.2–1 028.5°C under 3.37–5.08 kbar, whereas in basaltic andesite was 1 181.5–1 187.0°C under 1.79–4.46 kbar. Pyroxene compositions and invariable La/Sm vs La values of whole rock powders indicate that lavas were erupted in rapid cooling rate and mainly controlled by fractional crystallization (FC). In addition, oscillatory zonings in plagioclase and pyroxene phenocrysts indicated small local perturbations and degassing episodes in the magma chamber. Some high Mg# clinopyroxene antecrysts were found in EMB lavas. The highest Mg# of parental EMB melts is 69, which falls into the range of initial partial melts from upper mantle peridotite source (68–75). In terms of isotopic compositions, the EMB lavas most likely originated from Indian-type MORB mantle which was influenced by subduction components. In details, the subduction components are mainly derived from the dehydration of a subducted altered oceanic crust, and the contribution of sediment influence is minor. The Pb isotopic compositions and end member modeling further suggest that the source of subduction components is more likely from the Pacific Plate instead of the Solomon Plate.

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Acknowledgment

We appreciate LAI Zhiqing from the Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao, China for his efforts on our experiments. We also thank LIU Mu from the Research Institute of Uranium Geology, China National Nuclear Corporation, Beijing; YIN Xuebo from the Institute of Oceanology, Chinese Academy of Sciences; and LIANG Xinrong from the Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, for their help in XRF, ICP-MS, and MC-ICP-MS analyses. Meanwhile, we express our gratitude to the crews of the R/V Science during the Cruise 201501 for their efforts on obtaining samples. In addition, we appreciate the anonymous reviewers and Dr. CHEN for their careful work and thoughtful suggestions that have helped improve this paper substantially.

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  1. CAS Key Laboratory for Experimental Study under Deep-sea Extreme Conditions, Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, 572000, China

    Xia Zhao, Liyan Tian, Jianhui Sun, Yan Li & Yue Gao

  2. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China

    Xia Zhao & Peng Huang

  3. University of Chinese Academy of Sciences, Beijing, 100049, China

    Xia Zhao, Yan Li & Yue Gao

  4. Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, 266071, China

    Peng Huang

  5. Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China

    Peng Huang

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Correspondence to Peng Huang.

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The authors declare that the data supporting the findings of this study are available within the article and its electronic supplementary files. And the data in this study are also available from the authors upon reasonable request.

Supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (No. XDB42020303, XDA11030302), the National Natural Science Foundation of China (No. 41576055), and the National Basic Research Program of China (973 Program) (No. 2013CB429702)

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Zhao, X., Tian, L., Sun, J. et al. Petrogenesis of volcanic rocks from Eastern Manus Basin: indications in mineralogy and geochemistry. J. Ocean. Limnol. 39, 89–109 (2021). https://doi.org/10.1007/s00343-020-9308-1

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