Australian Plate
| Australian Plate | |
|---|---|
 | |
| Type | Major |
| Approx. Area | 47,000,000 km2[1] |
| Movement1 | north-east |
| Speed1 | 62-70mm/year |
| Features | Australia, New Guinea, New Zealand, Indian Ocean |
| 1Relative to the African Plate | |
The Australian Plate is a major tectonic plate in the eastern and, largely, in the southern hemispheres. Originally a part of the ancient continent of Gondwana, Australia remained connected to India and Antarctica until approximately 100 million years ago when India broke away and began moving north. Australia and Antarctica began rifting 85 million years ago and completely separated roughly 45 million years ago[2] The Australian plate later fused with the adjacent Indian Plate beneath the Indian Ocean to form a single Indo-Australian Plate. However, recent studies suggest that the two plates have once again split apart and have been separate plates for at least 3 million years and likely longer.[3] The Australian plate includes the continent of Australia, including Tasmania, as well portions of New Guinea, New Zealand, and the Indian Ocean basin.
Geography
The northeasterly side is a complex but generally convergent boundary with the Pacific Plate. The Pacific Plate is subducting under the Australian Plate, which forms the Tonga and Kermadec Trenches, and the parallel Tonga and Kermadec island arcs. It has also uplifted the eastern parts of New Zealand's North Island.
The continent of Zealandia, which separated from Australia 85 million years ago and stretches from New Caledonia in the north to New Zealand’s subantarctic islands in the south, is now being torn apart along the transform boundary marked by the Alpine Fault.
South of New Zealand the boundary becomes a transitional transform-convergent boundary, the Macquarie Fault Zone, where the Australian Plate is beginning to subduct under the Pacific Plate along the Puysegur Trench. Extending southwest of this trench is the Macquarie Ridge.
The southerly side is a divergent boundary with the Antarctic Plate called the Southeast Indian Ridge (SEIR).
The subducting boundary through Indonesia is not parallel to the biogeographical Wallace line that separates the indigenous fauna of Asia from that of Australasia. The eastern islands of Indonesia lie mainly on the Eurasian Plate, but have Australasian-related fauna and flora. Southeasterly lies the Sunda Shelf.
Origins
Depositional age of the Mount Barren Group on the southern margin of the Yilgarn Craton and zircon provenance analysis support the hypothesis that collisions between the Pilbara–Yilgarn and Yilgarn–Gawler Cratons assembled a proto-Australian continent approximately 1,696 million years ago (Dawson et al. 2002).[4]
References
- ↑ "Sizes of Tectonic or Lithospheric Plates". Geology.about.com. 2014-03-05. Retrieved 2015-12-25.
- ↑ "New Look at Gondwana's Breakup". Livescience.com. 2013-07-05. Retrieved 2015-12-25.
- ↑ Stein, Seth; Sella, Giovanni F.; Okai, Emile A. (2002). "The January 26, 2001 Bhuj Earthquake and the Diffuse Western Boundary of the Indian Plate" (PDF). American Geophysical Union. doi:10.1029/GD030p0243. Retrieved 2015-12-25.
- ↑ Dawson, Galvin C.; Krapež, Bryan; Fletcher, Ian R.; McNaughton, Neal J.; Rasmussen, Birger (2002). "Did late Palaeoproterozoic assembly of proto-Australia involve collision between the Pilbara, Yilgarn and Gawler Cratons? Geochronological evidence from the Mount Barren Group in the Albany–Fraser Orogen of Western Australia". Precambrian Research 118 (3-4): 195–220. doi:10.1016/S0301-9268(02)00110-9. ISSN 0301-9268. Retrieved 25 December 2015.
