Using the high-temperature phase transition of iron sulfide minerals as an indicator of fault slip temperature-Reference-Cited by-同舟云学术

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Using the high-temperature phase transition of iron sulfide minerals as an indicator of fault slip temperature

Published:2019-05-28 Issue:1 Volume:9 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Chen Yan-Hong,Chen Yen-Hua,Hsu Wen-Dung,Chang Yin-Chia,Sheu Hwo-Shuenn,Lee Jey-Jau,Lin Shih-Kang

Funder

Ministry of Science and Technology, Taiwan

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41598-019-44319-8.pdf

Reference37 articles.

1. Chang, L. et al. Identification and environmental interpretation of diagenetic and biogenic greigite in sediments: A lesson from the Messinian Black Sea. Geochemistry, Geophysics, Geosystems 15, 3612–3627 (2014).

2. Fu, C., Bloemendal, J., Qiang, X., Hill, M. J. & An, Z. Occurrence of greigite in the Pliocene sediments of Lake Qinghai, China, and its paleoenvironmental and paleomagnetic implications. Geochemistry, Geophysics, Geosystems 16, 1293–1306 (2015).

3. Chang, Y. S., Savitha, S., Sadhasivam, S., Hsu, C. K. & Lin, F. H. Fabrication, characterization, and application of greigite nanoparticles for cancer hyperthermia. Journal of Colloid and Interface Science 363, 314–319 (2011).

4. Nekrasov, I. J. & Besmen, N. I. Pyrite-pyrrhotite geothermometer. Distribution of cobalt, nickel and tin. Physics and Chemistry of the Earth 11, 767–771 (1979).

5. Aubourg, C. & Pozzi, J. P. Toward a new <250 °C pyrrhotite-magnetite geothermometer for claystones. Earth and Planetary Science Letters 294, 47–57 (2010).

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