Evolution of Paleogene Surtseyan volcanoes, primary eruption processes and post-eruptive bioclastic sedimentation. Chatham Island. New Zealand.

Leonor Sorrentino-Mariconda, Ray Cas, Jeffrey Stilwell

Research output: Contribution to conferenceAbstractOther

Abstract

The Chatham Islands archipelago is located 860km east of the South Island, New Zealand, and is situated on the eastern edge of the partially submerged continental plateau, the Chatham Rise. The group comprises two main islands, Chatham and Pitt, and a smaller set of islets, which have preserved a geologic record since the Permian.
Original languageEnglish
Pages74-74
Number of pages1
Publication statusPublished - 2008

Cite this

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title = "Evolution of Paleogene Surtseyan volcanoes, primary eruption processes and post-eruptive bioclastic sedimentation. Chatham Island. New Zealand.",
abstract = "The Chatham Islands archipelago is located 860km east of the South Island, New Zealand, and is situated on the eastern edge of the partially submerged continental plateau, the Chatham Rise. The group comprises two main islands, Chatham and Pitt, and a smaller set of islets, which have preserved a geologic record since the Permian.",
author = "Leonor Sorrentino-Mariconda and Ray Cas and Jeffrey Stilwell",
year = "2008",
language = "English",
pages = "74--74",

}

TY - CONF

T1 - Evolution of Paleogene Surtseyan volcanoes, primary eruption processes and post-eruptive bioclastic sedimentation. Chatham Island. New Zealand.

AU - Sorrentino-Mariconda, Leonor

AU - Cas, Ray

AU - Stilwell, Jeffrey

PY - 2008

Y1 - 2008

N2 - The Chatham Islands archipelago is located 860km east of the South Island, New Zealand, and is situated on the eastern edge of the partially submerged continental plateau, the Chatham Rise. The group comprises two main islands, Chatham and Pitt, and a smaller set of islets, which have preserved a geologic record since the Permian.

AB - The Chatham Islands archipelago is located 860km east of the South Island, New Zealand, and is situated on the eastern edge of the partially submerged continental plateau, the Chatham Rise. The group comprises two main islands, Chatham and Pitt, and a smaller set of islets, which have preserved a geologic record since the Permian.

M3 - Abstract

SP - 74

EP - 74

ER -