Nanogoethite as a Potential Indicator of Remagnetization in Red Beds-Reference-Cited by-同舟云学术

Nanogoethite as a Potential Indicator of Remagnetization in Red Beds

Published:2019-11-20 Issue:22 Volume:46 Page:12841-12850
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Huang Wentao¹²^ORCID,Jackson Michael J.³^ORCID,Dekkers Mark J.⁴^ORCID,Solheid Peat³,Zhang Bo⁵^ORCID,Guo Zhaojie⁵^ORCID,Ding Lin¹^ORCID

Affiliation:

1. Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing China

2. Department of Earth and Environmental Sciences University of Rochester Rochester NY USA

3. Institute for Rock Magnetism, Department of Earth Sciences University of Minnesota MN USA

4. Department of Earth Sciences Utrecht University Utrecht The Netherlands

5. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences Peking University Beijing China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084715

Reference41 articles.

1. Goethite stability and the origin of red beds

2. Low temperature magnetism and Mössbauer spectroscopy study from natural goethite

3. Magnetic properties of hematite nanoparticles

4. Insights into the early Tibetan Plateau from (U–Th)/He thermochronology

5. Transformation of Two-Line Ferrihydrite to Goethite and Hematite as a Function of pH and Temperature

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