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Tectonic implications of fault-scarp - derived volcaniclastic deposits on Macquarie Island: Sedimentation at a fossil ridge-transform intersection? Geological Society of America Bulletin, 2005 (Ref: 12403)
Authors:
Daczko N.R.Mosher S.Coffin M.F.Meckel T.A.
Category 1: Peer-reviewed literature

LAW DOME ATMOSPHERIC TRACE GAS RECORDS EXTENDED TO 2000 YEARS 8th International Global Atmosheric Chemistry Conference, Christchurch , NZ. September 2004, 2004 (Ref: 11835)
Authors:
MacFarling C.Etheridge D.van Ommen T.Steele P.Trudinger C.Langenfelds R.
Category 3: Abstract

High precision multispecies trace gas measurements of Law Dome ice have been produced for the last 2000 years. The new records of CO2 and CH4 compare very well with the published Law Dome records of the last 1000 years. The new measurements are used to confirm the changes observed in these records…

Macquarie Island's Finch-Langdon Fault Zone: A ridge-transform corner structure preserved along the pacific-Australian plate boundary Geological Society of America Abstracts with Programs, 2000 (Ref: 9367)
Authors:
Wertz K.Daczko N.R.Mosher S.Coffin M.F.
Category 3: Abstract

Macquarie Island, located along the Australian-Pacific transform plate boundary~1200 km south of New Zealand, consists of uplifted oceanic crust that still lies within the ocean basin where it formed. A lower crustal and upper mantle section of sheeted dikes…

Neotectonics of the Macquarie Ridge Complex, Australia-Pacific plate boundary Journal of Geophysical Research, 2000 (Ref: 9543)
Authors:
Massell C.Coffin M.F.Mann P.Mosher S.Frohlich C.Duncan C.S.Karner G.Ramsay D.Lebrun J.F.
Category 1: Peer-reviewed literature

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