சீலாந்தியா (Tamil Wikipedia)

Analysis of information sources in references of the Wikipedia article "சீலாந்தியா" in Tamil language version.

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cnn.com

crownminerals.govt.nz

doi.org

dx.doi.org

geosociety.org

gns.cri.nz

  • "The origin and meaning of the name Te Riu-a-Māui/Zealandia". www.gns.cri.nz. GNS Science. 2 May 2019. பார்க்கப்பட்ட நாள் 11 August 2020.
  • Wood, Ray; Stagpoole, Vaughan; Wright, Ian; Davy, Bryan; Barnes, Phil (2003). New Zealand's Continental Shelf and UNCLOS Article 76 (PDF). Institute of Geological and Nuclear Sciences series 56; NIWA technical report 123. Wellington, New Zealand: Institute of Geological and Nuclear Sciences Limited; National Institute of Water and Atmospheric Research. p. 16. Archived from the original (PDF) on 2007-02-21. பார்க்கப்பட்ட நாள் 22 பிப்ரவரி 2007. The continuous rifted basement structure, thickness of the crust, and lack of seafloor spreading anomalies are evidence of prolongation of the New Zealand land mass to Gilbert Seamount. {{cite book}}: Check date values in: |accessdate= (help)

mfe.govt.nz

  • "Figure 8.1: New Zealand in relation to the Indo-Australian and Pacific Plates". The State of New Zealand’s Environment 1997. 1997. Archived from the original on 2005-01-18. பார்க்கப்பட்ட நாள் 2007-04-20.

stuff.co.nz

teara.govt.nz

  • Keith Lewis; Scott D. Nodder; Lionel Carter (2007-01-11). "Zealandia: the New Zealand continent". Te Ara Encyclopedia of New Zealand. பார்க்கப்பட்ட நாள் 22 பிப்ரவரி 2007. {{cite web}}: Check date values in: |accessdate= (help)

telegraph.co.uk

theguardian.com

web.archive.org

  • "Figure 8.1: New Zealand in relation to the Indo-Australian and Pacific Plates". The State of New Zealand’s Environment 1997. 1997. Archived from the original on 2005-01-18. பார்க்கப்பட்ட நாள் 2007-04-20.
  • Wood, Ray; Stagpoole, Vaughan; Wright, Ian; Davy, Bryan; Barnes, Phil (2003). New Zealand's Continental Shelf and UNCLOS Article 76 (PDF). Institute of Geological and Nuclear Sciences series 56; NIWA technical report 123. Wellington, New Zealand: Institute of Geological and Nuclear Sciences Limited; National Institute of Water and Atmospheric Research. p. 16. Archived from the original (PDF) on 2007-02-21. பார்க்கப்பட்ட நாள் 22 பிப்ரவரி 2007. The continuous rifted basement structure, thickness of the crust, and lack of seafloor spreading anomalies are evidence of prolongation of the New Zealand land mass to Gilbert Seamount. {{cite book}}: Check date values in: |accessdate= (help)
  • "Great South Basin – Questions and Answers". 2007-07-11. Archived from the original on 2008-10-14. பார்க்கப்பட்ட நாள் 2008-04-18.
  • "New survey published on NZ mineral deposits". 30 May 2007. Archived from the original on 2008-10-16. பார்க்கப்பட்ட நாள் 2008-04-18.