FN Archimer Export Format
PT J
TI Zealandia: Earth’s Hidden Continent
BT 
AF Mortimer, Nick
   Campbell, Hamish J.
   Tulloch, Andy J.
   King, Peter R.
   Stagpoole, Vaughan M.
   Wood, Ray A.
   Rattenbury, Mark S.
   Sutherland, Rupert
   Adams, Chris J.
   Collot, Julien
   Seton, Maria
AS 1:1;2:2;3:1;4:2;5:2;6:2;7:2;8:3;9:1;10:4;11:5;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;
C1 GNS Science, Private Bag 1930, Dunedin 9054, New Zealand
   GNS Science, P.O. Box 30368, Lower Hutt 5040, New Zealand
   SGEES, Victoria University of Wellington, P.O. Box 600, Wellington 6140, New Zealand
   Service Géologique de Nouvelle Calédonie, B.P. 465, Nouméa 98845, New Caledonia
   School of Geosciences, University of Sydney, NSW 2006, Australia
C2 GNS SCIENCE, NEW ZEALAND
   GNS SCIENCE, NEW ZEALAND
   UNIV WELLINGTON VICTORIA, NEW ZEALAND
   SERV GEOL NOUVELLE CALEDONIE, FRANCE
   UNIV SYDNEY, AUSTRALIA
TC 0
UR https://archimer.ifremer.fr/doc/00489/60035/63303.pdf
LA English
DT Article
CR TECTA
BO L'Atalante
AB A 4.9 Mkm2 region of the southwest Pacific Ocean is made up of continental crust. The region has elevated bathymetry relative to surrounding oceanic crust, diverse and silica-rich rocks, and relatively thick and low-velocity crustal structure. Its isolation from Australia and large area support its definition as a continent— Zealandia. Zealandia was formerly part of Gondwana. Today it is 94% submerged, mainly as a result of widespread Late Cretaceous crustal thinning preceding supercontinent breakup and consequent isostatic balance. The identification of Zealandia as a geological continent, rather than a collection of continental islands, fragments, and slices, more correctly represents the geology of this part of Earth. Zealandia provides a fresh context in which to investigate processes of continental rifting, thinning, and breakup. 
PY 2017
PD MAR
SO GSA Today
SN 10525173
PU Geological Society of America
VL 27
IS 3
BP 27
EP 35
DI 10.1130/GSATG321A.1
ID 60035
ER

EF