| Tākaka Terrane | |
|---|---|
| Stratigraphic range: Cambrian-Devonian ~ | |
 | |
| Type | Terrane |
| Unit of | Austral Superprovince Western Province |
| Sub-units | Haupiri, Devil River Volcanics, Mount Patriarch, Mount Arthur, Ellis, Edgecumbe, Cameron & Pegasus Groups |
| Underlies | Tuhua Intrusive, Waka & Haerenga Supergroups |
| Lithology | |
| Primary | Sandstone, marble, basalt |
| Location | |
| Coordinates | 41°06′S 172°48′E / 41.1°S 172.8°E |
| Region | Tasman District |
| Country | New Zealand |
| Type section | |
| Named for | Tākaka Hill |
 Cross-section of New Zealand's stratigraphy | |
The Tākaka Terrane is a Paleozoic terrane that outcrops in the South Island of New Zealand. It is most extensively exposed within the Kahurangi National Park in the Tasman District. The terrane is mostly made up of marble and volcanic rocks but is highly variable in composition. It ranges in age from mid-Cambrian to Devonian time (510–400 Ma), including New Zealand's oldest rocks, which are found in the Cobb Valley in north-west Nelson. The Cobb Valley is also the location of "Trilobite Rock" a glacial dropstone made from the moulted exoskeletons of trilobites.[1] Asbestos was mined in the Cobb Valley from the Tākaka Terrene between the late 1880s and 1917. The Tākaka Terrane is highly deformed and has been intruded by many batholiths.
Description
The Tākaka Terrane has two main igneous units, the arc-related Devil River Volcanics Group (Middle to Late Cambrian) and the rift‐related Gendarme Dolerite (latest Cambrian to Early Ordovician age). The Devil River Volcanics Group sediments contain trilobites, brachiopods and conodonts. Sedimentary units in the Tākaka Terrane (Haupiri Group and Junction Formation rocks) likely formed in a back-arc basin.[2] The distinctive Arthur Marble from Tākaka Hill and Mount Arthur is of Ordovician age.[3] It has been speculated that the Tākaka Terrane is equivalent to rocks in Tasmania, Australia and was separated from them with the opening of the Tasman Sea.[4]
The Arthur Marble has been chemically weathered by rain and groundwater due to its high calcium carbonate content forming a karst geomorphology.[5][6] This has led to the formation of extensive cave systems like Harwoods Hole and the Riuwaka Resurgence.
See also
References
- ^ "Trilobite Rock". teara.govt.nz.
- ^ Münker, Carsten; Cooper, Roger (1999). "The Cambrian arc complex of the Takaka Terrane, New Zealand: An integrated stratigraphical, paleontological and geochemical approach". New Zealand Journal of Geology and Geophysics. 42 (3): 415–445. doi:10.1080/00288306.1999.9514854. ISSN 0028-8306.
- ^ Simes, John E. (1980). "Age of the Arthur Marble: conodont evidence from Mount Owen, northwest Nelson". New Zealand Journal of Geology and Geophysics. 23 (4): 529–532. doi:10.1080/00288306.1980.10424123. ISSN 0028-8306.
- ^ Cooper, R.A; Tulloch, A.J (1992). "Early Palaeozoic terranes in New Zealand and their relationship to the Lachlan Fold Belt". Tectonophysics. 214 (1–4): 129–144. Bibcode:1992Tectp.214..129C. doi:10.1016/0040-1951(92)90193-A. ISSN 0040-1951.
- ^ Williams, Paul W. (1987). "The Significance of Karst in New Zealand National Parks". New Zealand Geographer. 43 (2): 84–94. doi:10.1111/j.1745-7939.1987.tb01095.x. ISSN 0028-8144.
- ^ "New Zealand limestone country (Karst)". teara.govt.nz.
This page was last edited on 23 May 2024, at 07:22