Startseite Naturwissenschaften Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc
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Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc

  • Scott A. Whattam EMAIL logo , John W. Shervais , Mark K. Reagan , Daniel A. Coulthard , Julian A. Pearce , Peter Jones , Jieun Seo , Keith Putirka , Timothy Chapman , Daniel Heaton , Hongyan Li , Wendy R. Nelson , Kenji Shimizu und Robert J. Stern
Veröffentlicht/Copyright: 29. Oktober 2020
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American Mineralogist
Aus der Zeitschrift American Mineralogist Band 105 Heft 10

Abstract

Central aims of IODP Expedition 352 were to delineate and characterize the magmatic stratigraphy in the Bonin forearc to define key magmatic processes associated with subduction initiation and their potential links to ophiolites. Expedition 352 penetrated 1.2 km of magmatic basement at four sites and recovered three principal lithologies: tholeiitic forearc basalt (FAB), high-Mg andesite, and boninite, with subordinate andesite. Boninites are subdivided into basaltic, low-Si, and high-Si varieties. The purpose of this study is to determine conditions of crystal growth and differentiation for Expedition 352 lavas and compare and contrast these conditions with those recorded in lavas from mid-ocean ridges, forearcs, and ophiolites. Cr# (cationic Cr/Cr+Al) vs. TiO2 relations in spinel and clinopyroxene demonstrate a trend of source depletion with time for the Expedition 352 forearc basalt to boninite sequence that is similar to sequences in the Oman and other suprasubduction zone ophiolites. Clinopyroxene thermobarometry results indicate that FAB crystallized at temperatures (1142–1190 °C) within the range of MORB (1133–1240 °C). When taking into consideration liquid lines of descent of boninite, orthopyroxene barometry and olivine thermometry of Expedition 352 boninites demonstrate that they crystallized at temperatures marginally lower than those of FAB, between ~1119 and ~1202 °C and at relatively lower pressure (~0.2–0.4 vs. 0.5–4.6 kbar for FAB). Elevated temperatures of boninite orthopyroxene (~1214 °C for low-Si boninite and 1231–1264 °C for high-Si boninite) may suggest latent heat produced by the rapid crystallization of orthopyroxene. The lower pressure of crystallization of the boninite may be explained by their lower density and hence higher ascent rate, and shorter distance of travel from place of magma formation to site of crystallization, which allowed the more buoyant and faster ascending boninites to rise to shallower levels before crystallizing, thus preserving their high temperatures.

Keywords: International Ocean Discovery Program (IODP); JOIDES Resolution; Expedition 352; Izu-Bonin-Mariana Fore Arc; forearc basalt; boninite; ophiolite; Sites U1439; U1440; U1441; U1442; New Advances in Subduction Zone Magma Genesis

† Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.

Funding statement: S.A.W. acknowledges support from the Korea International Ocean Discovery Program (K-IODP) funded by the Ministry of Oceans and Fisheries, Korea. We also acknowledge support from NSF award OCE-1558689 (JWS) and OCE-1558688 (MKR). J.S. acknowledges support by the Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education (2016R1D1A3B03931481). T.C. acknowledges the Australia-New Zealand IODP consortium (ANZIC), which enabled participation on Exp. 352 and post-expedition funding via the support of government agencies and universities together with the ARC LIEF scheme (LE140100047). H.L. acknowledges support from the National Program on Global Change and Air-Sea Interaction (GASI-GEOGE-02).

Acknowledgments

This research used samples and data provided by the International Ocean Discovery Program (IODP). We thank the crew and scientific staff onboard Expedition 352, particularly Katarina Petronotis, for their excellent work. S.A.W. thanks T. Ishikawa for sharing compositional data of Semail ophiolite boninite minerals. We thank numerous anonymous reviewers whose suggestions greatly improved the manuscript.

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Received: 2018-05-17
Accepted: 2020-03-07
Published Online: 2020-10-29
Published in Print: 2020-10-27

© 2020 Walter de Gruyter GmbH, Berlin/Boston

Artikel in diesem Heft

  1. Roebling Medal Paper
  2. The effects of solid-solid phase equilibria on the oxygen fugacity of the upper mantle
  3. Structural and spectroscopic study of the kieserite-dwornikite solid-solution series, (Mg,Ni)SO4·H2O, at ambient and low temperatures, with cosmochemical implications for icy moons and Mars
  4. Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc
  5. An evolutionary system of mineralogy. Part II: Interstellar and solar nebula primary condensation mineralogy (>4.565 Ga)
  6. Swelling capacity of mixed talc-like/stevensite layers in white/green clay infillings (“deweylite”/“garnierite”) from serpentine veins of faulted peridotites, New Caledonia
  7. Experimental observations of TiO2 activity in rutile-undersaturated melts
  8. Direct evidence for the source of uranium in the Baiyanghe deposit from accessory mineral alteration in the Yangzhuang granite porphyry, Xinjiang Province, northwest China
  9. Extraction of high-silica granites from an upper crustal magma reservoir: Insights from the Narusongduo magmatic system, Gangdese arc
  10. “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” byAngel et al. (2017)—Discussion
  11. “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” —Reply to Zhong et al
  12. Letter
  13. Synthesis and crystal structure of Pb-dominant tourmaline
  14. Element loss to platinum capsules in high-temperature–pressure experiments
  15. New Mineral Names
  16. Book Review
  17. Book Review: Fundamental Planetary Science: Physics, Chemistry and Habitability
https://doi.org/10.2138/am-2020-6640
Schlagwörter für diesen Artikel
International Ocean Discovery Program (IODP); JOIDES Resolution; Expedition 352; Izu-Bonin-Mariana Fore Arc; forearc basalt; boninite; ophiolite; Sites U1439; U1440; U1441; U1442; New Advances in Subduction Zone Magma Genesis

Artikel in diesem Heft

  1. Roebling Medal Paper
  2. The effects of solid-solid phase equilibria on the oxygen fugacity of the upper mantle
  3. Structural and spectroscopic study of the kieserite-dwornikite solid-solution series, (Mg,Ni)SO4·H2O, at ambient and low temperatures, with cosmochemical implications for icy moons and Mars
  4. Mineral compositions and thermobarometry of basalts and boninites recovered during IODP Expedition 352 to the Bonin forearc
  5. An evolutionary system of mineralogy. Part II: Interstellar and solar nebula primary condensation mineralogy (>4.565 Ga)
  6. Swelling capacity of mixed talc-like/stevensite layers in white/green clay infillings (“deweylite”/“garnierite”) from serpentine veins of faulted peridotites, New Caledonia
  7. Experimental observations of TiO2 activity in rutile-undersaturated melts
  8. Direct evidence for the source of uranium in the Baiyanghe deposit from accessory mineral alteration in the Yangzhuang granite porphyry, Xinjiang Province, northwest China
  9. Extraction of high-silica granites from an upper crustal magma reservoir: Insights from the Narusongduo magmatic system, Gangdese arc
  10. “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” byAngel et al. (2017)—Discussion
  11. “EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry” —Reply to Zhong et al
  12. Letter
  13. Synthesis and crystal structure of Pb-dominant tourmaline
  14. Element loss to platinum capsules in high-temperature–pressure experiments
  15. New Mineral Names
  16. Book Review
  17. Book Review: Fundamental Planetary Science: Physics, Chemistry and Habitability
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