Widespread occurrence of silicate‐hosted magnetic mineral inclusions in marine sediments and their contribution to paleomagnetic recording

  • Liao Chang
    Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences Peking University Beijing China
  • Andrew P. Roberts
    Research School of Earth Sciences The Australian National University Canberra Australia
  • David Heslop
    Research School of Earth Sciences The Australian National University Canberra Australia
  • Akira Hayashida
    Department of Environmental Systems Science Doshisha University Kyotanabe Japan
  • Jinhua Li
    Paleomagnetism and Geochronology Laboratory, Key Laboratory of Earth's Deep Interior Institute of Geology and Geophysics, Chinese Academy of Sciences Beijing China
  • Xiang Zhao
    Research School of Earth Sciences The Australian National University Canberra Australia
  • Wei Tian
    Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences Peking University Beijing China
  • Qinghua Huang
    Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences Peking University Beijing China

書誌事項

公開日
2016-12
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1002/2016jb013109
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>Magnetic mineral inclusions occur commonly within other larger mineral phases in igneous rocks and have been demonstrated to preserve important paleomagnetic signals. While the usefulness of magnetic inclusions in igneous rocks has been explored extensively, their presence in sediments has only been speculated upon. The contribution of magnetic inclusions to the magnetization of sediments, therefore, has been elusive. In this study, we use transmission electron microscope (TEM) and magnetic methods to demonstrate the widespread preservation of silicate‐hosted magnetic inclusions in marine sedimentary settings. TEM analysis reveals detailed information about the microstructure, chemical composition, grain size, and spatial arrangement of nanoscale magnetic mineral inclusions within larger silicate particles. Our results confirm the expectation that silicate minerals can protect magnetic mineral inclusions from sulfate‐reducing diagenesis and increase significantly the preservation potential of iron oxides in inclusions. Magnetic inclusions should, therefore, be considered as a potentially important source of fine‐grained magnetic mineral assemblages and represent a missing link in a wide range of sedimentary paleomagnetic and environmental magnetic studies. In addition, we present depositional remanent magnetization (DRM) modeling results to assess the paleomagnetic recording capability of magnetic inclusions. Our simulation demonstrates that deposition of larger silicate particles with magnetic inclusions will be controlled by gravitational and hydrodynamic forces rather than by geomagnetic torques. Thus, even though these large silicates may contain ideal single‐domain particles, they cannot contribute meaningfully to paleomagnetic recording. However, smaller (e.g., silt‐ and clay‐sized) silicates with unidirectionally magnetized magnetic inclusions can potentially record a reliable DRM.</jats:p>

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