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

被引:71
作者
Chang, Liao [1 ,2 ]
Roberts, Andrew P. [2 ]
Heslop, David [2 ]
Hayashida, Akira [3 ]
Li, Jinhua [4 ]
Zhao, Xiang [2 ]
Tian, Wei [1 ]
Huang, Qinghua [1 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Lab Orogen Belts & Crustal Evolut, Beijing, Peoples R China
[2] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia
[3] Doshisha Univ, Dept Environm Syst Sci, Kyotanabe, Japan
[4] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earths Deep Interior, Paleomagnetism & Geochronol Lab, Beijing, Peoples R China
基金
澳大利亚研究理事会; 中国国家自然科学基金;
关键词
DEPOSITIONAL REMANENT MAGNETIZATION; SINGLE PLAGIOCLASE CRYSTALS; REVERSAL CURVE DIAGRAMS; EXSOLVED MAGNETITE; ROCK MAGNETISM; NEW-ZEALAND; DISSOLUTION; DIAGENESIS; PARTICLES; INTRUSION;
D O I
10.1002/2016JB013109
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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.
引用
收藏
页码:8415 / 8431
页数:17
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