Dorsal de Reykjanes (Portuguese Wikipedia)

Analysis of information sources in references of the Wikipedia article "Dorsal de Reykjanes" in Portuguese language version.

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T. Petit, H. Mercier, V. Thierry (dezembro de 2019). New Insight Into the Formation and Evolution of the East Reykjanes Ridge Current and Irminger Current. Journal of Geophysical Research – Oceans. [S.l.: s.n.] doi:10.1029/2019JC015546

Ármann Höskuldsson, Richard Hey, Ferdinando Martinez, Ásdís Benediktsdóttir (janeiro de 2010). «Njörður central volcano, first direct evidence of shallow magma chambers on the Reykjanes ridge» (PDF) (em inglês). p. 79–80. Consultado em 22 abril 2021. Cópia arquivada (PDF) em 15 novembro 2012. Njörður central volcano, is situated at the foot of the Icelandic shelf on the Reykjanes ridge with its centre at 62.8°N and 25°V. Graben structures are not observed between 59°N and Njörður (62.8°N), as the Reykjanes ridge forms a topographic high along this part of the plate boundary.

Richard A. Lovett: Giant Undersea Volcano Found Off Iceland In: National Geographic News, 22 abril 2008.

Ármann Höskuldsson, Richard Hey, Ferdinando Martinez, Ásdís Benediktsdóttir (janeiro de 2010). «Njörður central volcano, first direct evidence of shallow magma chambers on the Reykjanes ridge» (PDF) (em inglês). p. 79–80. Consultado em 22 abril 2021. Cópia arquivada (PDF) em 15 novembro 2012. Njörður central volcano, is situated at the foot of the Icelandic shelf on the Reykjanes ridge with its centre at 62.8°N and 25°V. Graben structures are not observed between 59°N and Njörður (62.8°N), as the Reykjanes ridge forms a topographic high along this part of the plate boundary.