Anisotropy of Magnetic Susceptibility (AMS) of Sediments From Holes U1480E and U1480H, IODP Expedition 362: Sedimentary or Artificial Origin and Implications for Paleomagnetic Studies-Reference-Cited by-同舟云学术

Anisotropy of Magnetic Susceptibility (AMS) of Sediments From Holes U1480E and U1480H, IODP Expedition 362: Sedimentary or Artificial Origin and Implications for Paleomagnetic Studies

Published:2019-11 Issue:11 Volume:20 Page:5192-5215
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Yang Tao¹²^ORCID,Zhao Xixi³⁴,Petronotis Katerina⁵^ORCID,Dekkers Mark J.²^ORCID,Xu Huiru¹^ORCID

Affiliation:

1. Hubei Subsurface Multi‐Scale Imaging Key Laboratory Institute of Geophysics and Geomatics, China University of Geosciences Wuhan China

2. Paleomagnetic Laboratory Fort Hoofddijk, Department of Earth Sciences Utrecht University Utrecht Netherlands

3. State Key Laboratory of Marine Geology Tongji University Shanghai China

4. Department of Earth and Planetary Sciences University of California Santa Cruz CA USA

5. International Ocean Discovery Program Texas A&M University College Station TX USA

Funder

National Natural Science Foundation of China

Division of Earth Sciences

Division of Ocean Sciences

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008721

Reference71 articles.

1. Paleomagnetic overprints in ocean sediment cores and their relationship to shear deformation caused by piston coring

2. Coring-induced magnetic fabric in piston cores from the western Mediterranean

3. Data report: revised age models for IODP Sites U1480 and U1481, Expedition 362

4. Correlation of strain with anisotropy of magnetic susceptibility (AMS)

5. Statistics of Earth Science Data

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