Dun Mountain-Maitai Terrane

  (Redirected from Dun Mountain Ophiolite Belt)

The Dun Mountain-Maitai Terrane comprises the Dun Mountain Ophiolite Belt (also called the Mineral Belt), Maitai Group and Patuki Mélange.[1] The Dun Mountain Ophiolite is an ophiolite of Permian age located in New Zealand's South Island. Prehistorically this ophiolite was quarried by Māori for both metasomatized argillite and pounamu (jade) which was used in the production of tools and jewellery.[2]

Dun Mountain-Maitai Terrane
Stratigraphic range: Early Permian-Triassic
~280–200 Ma
Dun mountain Nelson New Zealand.jpg
View of Dun Mountain, name-giver to the terrane
TypeTerrane
Unit ofAustral Superprovince
Sub-unitsDun Mountain Ultramafics, Livingstone Volcanic & Maitai Groups, Otanomomo Complex
UnderliesMurihiku Terrane, Momotu & Haerenga Supergroups
OverliesCaples Terrane
Lithology
PrimaryBasalt, gabbro, peridotite, sedimentary rocks
OtherJade
Location
RegionNelson, Tasman, Marlborough, Otago & Southland Regions
Country New Zealand
Type section
Named forDun Mountain & Maitai River

In the late 1800s, the Dun Mountain Ophiolite Belt was surveyed for its economic potential. During this time the rock types dunite and rodingite (after Dun Mountain and the Roding River) were first named.[3] Discovery of economic deposits of chromite near Nelson lead to the building of New Zealand’s first railway, however, extraction only occurred between 1862 and 1866. In the 20th century, serpentinite was mined for fertiliser and the ophiolite remains one of New Zealand's main sources of pounamu (jade), but all other mineral exploration has failed to find economic deposits.

DescriptionEdit

 
Maitai Group sediments folded into an isoclinal syncline

The Dun Mountain Ophiolite Belt is composed of a typical ophiolite sequence of ultramafic rocks overlain by a plutonic then volcanic sequence, and finally by conglomerates and other sedimentary rocks of the Maitai Group. The unaltered ultramafic rocks are restricted to three massifs, Dun Mountain, the Red Hills and Red Mountain, elsewhere they are highly serpentinized. This ophiolite sequence is structurally underlain by the ophiolitic Patuki Mélange. The Dun Mountain Ophiolite Belt likely formed in a forearc environment.[4]

  • Mantle lithologies
    • Dun Mountain Ultramafics Group
    • Wairere Serpentinite
    • Upukerora Mélange
  • Crustal igneous rocks
    • Otanomomo Complex
    • Livingstone Volcanics Group
  • Crustal sedimentary rock
    • Maitai Group
      • Upukerora Breccia
      • Wooded Peak Limestone
      • Tramway Sandstone
      • Greville Formation
      • Little Ben Sandstone
      • Stephens Subgroup
  • Basal mélange
    • Windon Mélange
    • Paruki Mélange

DistributionEdit

 
Vegetation change from the Dun Mountain Ophiolite Belt ultramafic rock (left) to mafic and sedimentary rock on the right.[5]

The Dun Mountain Ophiolite Belt is a locally intact approximately 12 kilometres (7.5 mi) section through oceanic crust.[6] It is exposed between D'Urville Island in Marlborough District and St Arnaud in Tasman District, and Jackson Bay in the West Coast Region and Balclutha in Otago. The Dun Mountain Ophiolite Belt is exposed in the South Island and is inferred to exist at depth under the North Island. It is in two sections, as it is offset by the Alpine Fault, with sections to the west of the fault having been displaced northwards. The Dun Mountain-Maitai Terrane also extends at depth into the North Island as far as Northland.[7]

See alsoEdit

ReferencesEdit

  1. ^ Mortimer, N; Rattenbury, MS; King, PR; Bland, KJ; Barrell, DJA; Bache, F; Begg, JG; Campbell, HJ; Cox, SC; Crampton, JS; Edbrooke, SW; Forsyth, PJ; Johnston, MR; Jongens, R; Lee, JM; Leonard, GS; Raine, JI; Skinner, DNB; Timm, C; Townsend, DB; Tulloch, AJ; Turnbull, IM; Turnbull, RE (2014). "High-level stratigraphic scheme for New Zealand rocks". New Zealand Journal of Geology and Geophysics. 57 (4): 402–419. doi:10.1080/00288306.2014.946062. ISSN 0028-8306.
  2. ^ Walls, J. Y. (1974). "Argillite quarries of the Nelson mineral belt". New Zealand Archaeological Association Newsletter. 7 (1): 37–43.
  3. ^ Johnston, M. R. (2007). "Nineteenth-century observations of the Dun Mountain Ophiolite Belt, Nelson, New Zealand and trans-Tasman correlations,". Geological Society, London, Special Publications. 287: 375–387. Bibcode:2007GSLSP.287..375J. doi:10.1144/sp287.27.
  4. ^ "New Zealand Geology: an illustrated guide" (PDF). www.geotrips.org.nz.
  5. ^ Robinson, Brett H.; Brooks, Robert R.; Kirkman, John H.; Gregg, Paul E.H.; Gremigni, Patrizia (1996). "Plant‐available elements in soils and their influence on the vegetation over ultramafic ("serpentine") rocks in New Zealand". Journal of the Royal Society of New Zealand. 26 (4): 457–468. doi:10.1080/03014223.1996.9517520. ISSN 0303-6758.
  6. ^ Coombs, D. S. (1976). "The Dun Mountain ophiolite belt, New Zealand, its tectonic setting, constitution, and origin, with special reference to the southern portion,". American Journal of Science. 276: 561–603. doi:10.2475/ajs.276.5.561.
  7. ^ Spörli, K. B.; Black, P. M.; Lindsay, J. M. (2015). "Excavation of buried Dun Mountain–Maitai terrane ophiolite by volcanoes of the Auckland Volcanic field, New Zealand". New Zealand Journal of Geology and Geophysics. 28 (3): 229–243.

External linksEdit