Rittmann volcano, Antarctica as the source of a widespread 1252 ± 2 CE tephra layer in Antarctica ice

Author:

Lee Mi Jung,Kyle Philip R.ORCID,Iverson Nels A.,Lee Jong Ik,Han Yeongcheol

Funder

National Science Foundation

Korea Polar Research Institute

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference44 articles.

1. Tephrochronology;Alloway,2013

2. Petrography and chemistry of lavas and comagmatic xenoliths of Mt. Rittmann, a volcano discovered during the IV Italian expedition in Northern Victoria Land (Antarctica);Armienti;Mem. Soc. Geol. Ital.,1991

3. The Ross Sea Dipole–temperature, snow accumulation and sea ice variability in the Ross Sea region, Antarctica, over the past 2700 years;Bertler;Clim. Past,2018

4. Fumarolic activity at Mt Rittmann volcano, northern Victoria Land, Antarctica;Bonaccorso;Mem. Soc. Geol. Ital.,1991

5. Late Pleistocene-Holocene volcanic activity in northern Victoria Land recorded in Ross Sea (Antarctica) marine sediments;Del Carlo;Bull. Volcanol.,2015

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