Physical interpretation of isothermal remanent magnetization end-members: New insights into the environmental history of Lake Hovsgul, Mongolia

Author:

Fabian Karl12ORCID,Shcherbakov Valeriy P.34ORCID,Kosareva Lina4ORCID,Nourgaliev Danis4ORCID

Affiliation:

1. Geological Survey of Norway; Trondheim Norway

2. Department of Geology; University of Tromsø; Tromsø Norway

3. Geophysical Observatory “Borok” of Russian Academy of Sciences; Borok Yaroslvaskaya oblast Russia

4. Institute of Geology and Petroleum Technologies, Kazan (Volga Region) Federal University; Kazan Russia

Funder

the Norwegian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference41 articles.

1. Controlled biomineralization of magnetite (Fe3O4) and greigite (Fe3S4) in a magnetotactic bacterium;Bazylinski;Appl. Environ. Microbiol.,1995

2. Belokon , V. V. Kochegura L. Sholpo 1973 Metody paleomagnitnykh issledovanii gornykh porod (Methods of Paleomagnetic Studies of Rocks)

3. Burov , B. D. Nurgaliev P. Yasonov 1986 Paleomagnetic Analysis

4. Identification and environmental interpretation of diagenetic and biogenic greigite in sediments: A lesson from the Messinian Black Sea;Chang;Geochem. Geophys. Geosyst.,2014

5. Geomagnetic secular variation recorded in the stable magnetic remanence of recent sediments;Creer;Earth Planet. Sci. Lett.,1972

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