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- Q17014968 subject Q8487986.
- Q17014968 subject Q8843734.
- Q17014968 abstract "The Narooma Accretionary Complex or Narooma Terrane is a geological structural region on the south coast of New South Wales, Australia that is the remains of a subduction zone or an oceanic terrane. It can be found on the surface around Narooma, Batemans Bay and down south into Victoria near Mallacoota.It has attached itself to the Lachlan Fold Belt and has been considered as either an exotic terrane or as a part of the fold belt. Rocks are turbidites, block in matrix mélange, chert, and volcanics. The accretionary complex itself could either be the toe of a subduction zone, or an accretionary prism.It was moved by the Pacific Plate westwards for about 2500 km until it encountered the east coast of Gondwana.It is part of the Mallacoota Zone according to Willman, which in turn is part of the Eastern Lachlan Fold Belt, which is part of the Benambra Terrane.".
- Q17014968 thumbnail Narooma_Breccia.JPG?width=300.
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- Q17014968 wikiPageWikiLink Q8487986.
- Q17014968 wikiPageWikiLink Q8843734.
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- Q17014968 comment "The Narooma Accretionary Complex or Narooma Terrane is a geological structural region on the south coast of New South Wales, Australia that is the remains of a subduction zone or an oceanic terrane. It can be found on the surface around Narooma, Batemans Bay and down south into Victoria near Mallacoota.It has attached itself to the Lachlan Fold Belt and has been considered as either an exotic terrane or as a part of the fold belt.".
- Q17014968 label "Narooma Terrane".
- Q17014968 depiction Narooma_Breccia.JPG.