Knowledge (XXG)

Australian Plate

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1799: 738:, which ends in the south as a long series of transform faults between the two plates called the Macquarie Ridge Complex, commencing with the McDougall Fault Zone and ending with the Macquarie Fault Zone. The south western portion of the zone has the Pacific Plate interacting with an area of the Australian Plate that the latest tectonic models suggest is still independent from when it first achieved independent rotation to the then Indo-Australian Plate several million years ago, the Macquarie microplate. 555: 2421: 2445: 2433: 613:. Due to vector complexities at the north eastern end of this collision, which includes several spreading centres, it is perhaps simplest to state that the average displacement rate to the north is about half that of the collision with the Sunda Plate, but this would not explain some of the largest and most destructive recent earthquakes and eruptions on the face of the planet. 29: 2457: 411:
which implies this area presently is weaker tectonically than the area where originally the Indian and Australian plates merged which is believed to have been further to the north west. There is also deformation in an approximately 1,200 km (750 mi) zone north of the Southeast Indian Ridge
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In terms of the middle of India and Australia landmasses, with Australia as the point of reference, presently Australia is moving northward at 3 cm (1.2 in) per year with respect to India consistent with a zone of deformation between the two plates as commented upon earlier. This zone of
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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
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Technically movement is a vector and requires to be related to something. Much of the work involved in determining these plate vectors involves assurance that the points of reference are representative of the plates they are on, as distortion will be likely in areas of tectonic activity. Further
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of 80° (slightly north of due east, at the Amsterdam transform fault to the south western side of Australian Plate), 7 cm (2.8 in) per year with heading 120° (southeast) and 6.6 cm (2.6 in) per year near the Macquarie Triple Junction which is the south eastern side of the
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and the south western aspects of the Pacific Plate. The Pacific Plate east to west convergence rates along the subduction systems with the Kermadec Plate, which are perhaps simpler to state, are among the fastest on Earth, being 8 cm (3.1 in) per year in the north and 4.5 cm
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There is oblique convergence of what are now the Pacific and Australian plates at about 11 cm/year (4.3 in/year) near eastern Papua New Guinea. This has resulted in shear complexities, resolved by the formation of multiple microplates and convergence velocity that varies between
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the subduction component of the Pacific Plate moving westward is about 3.9 cm (1.5 in) per year. The Australian Plate then to the south starts subducting under the Pacific Plate at a rate of 3.6 cm/year (1.4 in/year) at the
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Delescluse, Matthias; Chamot-Rooke, Nicolas; Cattin, Rodolphe; Fleitout, Luce; Trubienko, Olga; Vigny, Christophe (26 September 2012). "April 2012 intra-oceanic seismicity off Sumatra boosted by the Banda-Aceh megathrust".
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assumptions such as there are only 8 plates were made in earlier modelling when as many as 52 may exist, with independent movement, although fair accuracy for larger plate movement can be obtained if only 25 are modelled.
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to the south of New Zealand. There is up to 9.6 cm (3.8 in) per year motion accommodated with complex rotational components in the collision dynamics between the north eastern Australian Plate and the rotating
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The Capricorn plate at the western side of the Australian plate is moving at 1.9 mm (0.075 in) per year ± 0.5 mm (0.020 in) per year with heading 45° (northwest) relative to the Australia plate.
542:. The separation continued with various authors modelling full separation time based on sea levels and/or biological separation. A currently widely used reference model for plate movement has total separation of 566:
The Australian Plate, which Australia is on, is moving faster than other plates. The Australian Plate is moving about 6.9 cm (2.7 inches) a year in a northward direction and with a small clockwise rotation. The
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The eastern collision with the Pacific Plate has increasing displacement rates towards the north from a low of less than 0.2 cm (0.079 in) per year at the southern end of the
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Li, M; Huang, S; Hao, T; Dong, M; Xu, Y; Zhang, J; He, Q; Fang, G (2023). "Neogene subduction initiation models in the western Pacific and analysis of subduction zone parameters".
672:. The Australian Plate interacts at the southern and south-eastern border of the North Fiji Basin with the microplates of the New Hebrides already mentioned, as well as with the 741:
Data from the 11,800 km (7,300 mi) long Southeast Indian Ridge only became available after about 1985 and this gives a fairly consistent spreading rate between the
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data indicating that India and Australia are not moving on the same vectors northward and have started a process of again separating. This zone is along the northern
264:. It is however known from movement studies that this definition of the Australian Plate is 20% less accurate than one that assumes independently moving 1721: 1429:"Texture, mineralogy and geochemistry of hydrothermally altered submarine volcanics recovered southeast of Cheshire Seamount, western Woodlark Basin" 783: 1337: 1662:
Gasperini, L; Ligi, M; Accettella, D; Bosman, A; Cuffaro, M; Lodolo, E; Martorelli, E; Muccini, F; Palmiotto, C; Polonia, A (1 February 2023).
696:. The back arc spreading in the Lau Basin continues almost due south in the line of interaction between the Australian and Tonga plates to the 1396: 653:
to 4 cm/year (1.6 in/year) in the central section of the trench, to rise again to 12 cm/year (4.7 in/year) in the south.
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Yue, H.; Lay, T.; Koper, K. (2012). "En Ă©chelon and orthogonal fault ruptures of the 11 April 2012 great intraplate earthquakes".
773: 763: 333: 798: 693: 2498: 1714: 590:) has a maximum convergence velocity of 7.3 cm (2.9 in) per year ± 0.8 cm (0.31 in) per year at the 1552:"Seismic velocity structure and deformation due to the collision of the Louisville Ridge with the Tonga-Kermadec Trench" 793: 788: 768: 626: 1216: 2461: 2068: 1217:"Early Earth evolution: evidence from the 3.5–1.8 Ga geological history of the Pilbara region of Western Australia" 2108: 606: 568: 559: 269: 2483: 2449: 1707: 1594: 546:
by 60 million years ago although some had argued historically that this was as recent as 45 million years ago.
2437: 2341: 2168: 2003: 1963: 1895: 1807: 1738: 642: 39: 1622:"The kinematic evolution of the Macquarie Plate: A case study for the fragmentation of oceanic lithosphere" 1510: 2394: 2356: 2351: 2088: 705: 431: 371: 1761: 1550:
Stratford, W.; Peirce, C.; Paulatto, M.; Funnell, M.; Watts, A. B.; Grevemeyer, I.; Bassett, D. (2015).
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where the edge of the Australian plate makes a transition in a bend up towards the north-east via the
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while the subduction of the oceanic crust of the Australian Plate occurs to the south east in the
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decreasing to 6.0 cm (2.4 in) ± 0.04 cm (0.016 in) per year at the southern
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South of New Zealand the boundary becomes a transitional transform-convergent boundary, the
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when India broke away and began moving north. Australia and Antarctica had begun rifting by
952:"The January 26, 2001 Bhuj Earthquake and the Diffuse Western Boundary of the Indian Plate" 927: 2366: 2329: 2264: 2251: 2148: 1983: 1978: 1933: 1923: 1913: 1830: 1751: 1730: 1236: 742: 735: 661: 610: 447: 413: 367: 356: 352: 293: 265: 253: 126: 629:. To the south of this there is sea floor spreading between the Australian Plate and the 1679: 1526: 1487: 1444: 1314: 1267: 1177: 1126: 1075: 1029: 864:"The breakup history of Gondwana and its impact on pre-Cenozoic floristic provincialism" 2425: 2289: 2241: 2196: 2158: 2113: 2013: 1953: 1903: 1835: 1756: 718: 697: 650: 634: 630: 595: 587: 506: 470: 466: 462: 454: 443: 389: 351:, where the Australian Plate is beginning to subduct under the Pacific Plate along the 241: 106: 1322: 1275: 2477: 2404: 2236: 2226: 2221: 2211: 2201: 2186: 2103: 2073: 2043: 2028: 2018: 1993: 1988: 1885: 1860: 1820: 1815: 1783: 1746: 1509:
Roger, J; Pelletier, B; Gusman, A; Power, W; Wang, X; Burbidge, D; Duphil, M (2023).
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a deformation zone between the Indian and Australian Plates with both earthquake and
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Major tectonic plate separated from Indo-Australian Plate about 3 million years ago
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continues to be studied for clues as to the commencement and subsequent course of
1452: 2379: 2374: 2304: 2279: 2274: 2143: 2138: 2133: 2083: 2038: 2033: 1973: 1938: 1880: 1850: 1840: 1825: 803: 730: 714: 701: 689: 591: 583: 393: 385: 217: 209: 185: 81: 1648: 2259: 2216: 1535: 1495: 532: 304: 288:. The Pacific Plate is subducting under the Australian Plate, which forms the 233: 205: 181: 77: 28: 1460: 1406: 1388: 1283: 2231: 1664:"Late Miocene to recent tectonic evolution of the Macquarie Triple Junction" 681: 517: 502: 319: 237: 213: 73: 1193: 1142: 512:
As a separate plate the Australian Plate came into being on the breakup of
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and completely separated a while after this, some believing as recently as
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Report on the Asia Pacific Reference Frame (APREF) Project. Record 2019/17
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Depositional age of the Mount Barren Group on the southern margin of the
425: 177: 118: 1185: 1134: 392:, but have Australasian-related fauna and flora. Southeasterly lies the 1060:"Instantaneous deformation and kinematics of the India–Australia Plate" 966: 482: 461:
provenance analysis support the hypothesis that collisions between the
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The continental crust of this plate covers the whole of Australia, the
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where direct interaction resumes with the Pacific Plate south of the
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must be updated due to the movement, as some locations move faster.
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Choi, H; Kim, SS; Dyment, J.; Granot, R; Park, SH; Hong, JK (2017).
961:. Geodynamics Series. American Geophysical Union. pp. 243–254. 879: 537: 323: 152: 145: 138: 1699: 1299:"A synopsis of events related to the assembly of eastern Gondwana" 553: 297: 377:
The subducting boundary through Indonesia is not parallel to the
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and Australian Plates of 6 cm (2.4 in) per year at a
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with final separation from what is now the Antarctic Plate and
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deformation may actually presently involve some of India.
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hemispheres. Originally a part of the ancient continent of
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Vishiti, A.; Petersen, S.; Suh, C.E.; Devey, C.W. (2014).
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The northwards collision of the Australian Plate with the
307:. It has also uplifted the eastern parts of New Zealand's 1383:(Report). Canberra: GeoScience Australia. pp. 1–42. 384:
that separates the indigenous fauna of Asia from that of
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A Continent on the Move: New Zealand Geoscience Revealed
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Australia Is Not as Down Under as Everyone Thinks It Is
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To the east of Indonesia there appears to be under the
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Hickman and Van Kranendonk, Arthur and Martin (2012).
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2–48 cm/year (0.79–18.90 in/year) where the
240:. The Australian Plate is bordered (clockwise) by the 950:
Stein, Seth; Sella, Giovanni; Okai, Emile A. (2002).
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assembled a proto-Australian continent approximately
388:. The eastern islands of Indonesia lie mainly on the 1058:
Delescluse, Matthias; Chamot-Rooke, Nicolas (2007).
2365: 2250: 2167: 1894: 1806: 1737: 692:under which the Pacific Plate is subducting in the 586:(Sundaland Plate, previously classified as part of 216:. The continental crust also includes northwestern 160:The Australian plate later fused with the adjacent 69: 61: 53: 45: 35: 21: 280:The northeasterly side is a complex but generally 1338:"Australia Is Drifting So Fast GPS Can't Keep Up" 1107: 1105: 1103: 1053: 1051: 1049: 857: 855: 336:in the south, is now being torn apart along the 837:. Geology.about.com. 2014-03-05. Archived from 806: â€“ Tectonic plate including Southeast Asia 708:and such direct interaction continues into the 490:Australia and East Antarctica were merged with 49:47,000,000 km (18,000,000 sq mi) 558:Global plate tectonic movement as measured by 412:between the Australian Plate and the proposed 1715: 8: 1007: 1005: 1003: 1001: 999: 997: 995: 993: 928:"ODSN Plate Tectonic Reconstruction Service" 355:. Extending southwest of this trench is the 945: 943: 228:. The oceanic crust includes the southeast 2432: 1722: 1708: 1700: 1336:Howard, Brian Clark (September 23, 2016). 835:"Sizes of Tectonic or Lithospheric Plates" 656:Very active spreading then resumes in the 27: 1687: 1570: 1534: 1515:Natural Hazards and Earth System Sciences 1362:" by Michelle Innis, September 23, 2016, 1235: 1083: 1037: 1012:DeMets, C; Gordon, RG; Argus, DF (2010). 898: 896: 826: 784:List of earthquakes in Papua New Guinea 922: 920: 18: 1599:. Geoscience Society of New Zealand. 722:(1.8 in) per year in the south. 7: 2456: 1376:Hu, G.; Jia, M.; Dawson, J. (2019). 1014:"Geologically current plate motions" 1629:Earth and Planetary Science Letters 1348:from the original on Feb 27, 2021. 779:List of earthquakes in New Zealand 405:global satellite navigation system 334:New Zealand's subantarctic islands 121:, Australia remained connected to 14: 1559:Geophysical Journal International 1064:Geophysical Journal International 1018:Geophysical Journal International 605:, where there is the major plate 2455: 2444: 2443: 2431: 2419: 1797: 1085:10.1111/j.1365-246X.2006.03181.x 1039:10.1111/j.1365-246X.2009.04491.x 904:"New Look at Gondwana's Breakup" 774:List of earthquakes in Indonesia 764:List of earthquakes in Australia 1237:10.18814/epiiugs/2012/v35i1/028 2347:South American–Antarctic Ridge 1252:Orogen of Western Australia". 799:List of earthquakes in Vanuatu 694:Kermadec-Tonga subduction zone 1: 1323:10.1016/S0040-1951(02)00629-7 1276:10.1016/S0301-9268(02)00110-9 906:. Livescience.com. 2013-07-05 1476:Science China Earth Sciences 1453:10.1016/j.margeo.2013.11.002 868:Australian Journal of Botany 794:List of earthquakes in Tonga 789:List of earthquakes in Samoa 769:List of earthquakes in India 2494:Geology of the Indian Ocean 688:and the clockwise rotating 627:New Britain subduction zone 442:years ago. Accordingly the 2515: 2489:Natural history of Oceania 2300:Galápagos Spreading Center 1649:10.1016/j.epsl.2017.08.035 423: 2413: 1795: 1536:10.5194/nhess-23-393-2023 1496:10.1007/s11430-022-1065-1 625:and Pacific Plate at the 607:Macquarie Triple Junction 569:Global Positioning System 180:, as well as portions of 91: 26: 1389:10.11636/Record.2019.017 362:The southerly side is a 2342:Pacific-Antarctic Ridge 1641:2017E&PSL.478..132C 862:McLoughlin, S. (2001). 643:Vanuatu subduction zone 540: million years ago 529: million years ago 499: million years ago 485: million years ago 326: million years ago 318:, which separated from 155: million years ago 148: million years ago 141: million years ago 134: million years ago 2395:Pacific-Farallon Ridge 2367:Ancient oceanic ridges 2357:Southwest Indian Ridge 2352:Southeast Indian Ridge 2089:Philippine Mobile Belt 1593:Graham, I. J. (2015). 563: 487:(Dawson et al. 2002). 432:Eastern Pilbara Craton 372:Southeast Indian Ridge 1297:Meert, J. G. (2003). 810:Indo-Australian Plate 609:with the Pacific and 557: 531:and finishing in the 430:It is known that the 170:Indo-Australian Plate 2499:Geology of Australia 2270:Central Indian Ridge 1255:Precambrian Research 959:Plate Boundary Zones 710:Macquarie Fault Zone 678:Balmoral Reef Plates 666:Hunter Fracture Zone 623:South Bismarck Plate 603:Macquarie Fault Zone 349:Macquarie Fault Zone 129:until approximately 2385:Kula-Farallon Ridge 1680:2023Geo....51..146G 1527:2023NHESS..23..393R 1488:2023ScChD..66..472L 1445:2014MGeol.347...69V 1342:National Geographic 1315:2003Tectp.362....1M 1268:2002PreR..118..195D 1186:10.1038/nature11492 1178:2012Natur.490..245Y 1135:10.1038/nature11520 1127:2012Natur.490..240D 1076:2007GeoJI.168..818D 1030:2010GeoJI.181....1D 706:TaupĹŤ Volcanic Zone 639:New Hebrides Trench 621:subducts under the 434:within present day 328:and stretches from 296:, and the parallel 282:convergent boundary 202:Gulf of Carpentaria 2426:Geology portal 2400:Pacific-Kula Ridge 2390:Mid-Labrador Ridge 2315:Mid-Atlantic Ridge 2310:Juan de Fuca Ridge 1572:10.1093/gji/ggu475 967:10.1029/GD030p0243 750:Australian Plate. 647:New Hebrides Plate 564: 364:divergent boundary 338:transform boundary 2471: 2470: 2285:East Pacific Rise 1398:978-1-925848-54-0 1172:(7419): 245–249. 674:Conway Reef Plate 619:Solomon Sea Plate 436:Western Australia 409:Ninety East Ridge 314:The continent of 294:Kermadec Trenches 168:to form a single 99: 98: 2506: 2459: 2458: 2447: 2446: 2435: 2434: 2424: 2423: 2325:Kolbeinsey Ridge 1801: 1724: 1717: 1710: 1701: 1694: 1693: 1691: 1689:10.1130/G50556.1 1659: 1653: 1652: 1626: 1617: 1611: 1610: 1590: 1584: 1583: 1581: 1579: 1574: 1565:(3): 1503–1522. 1556: 1547: 1541: 1540: 1538: 1506: 1500: 1499: 1471: 1465: 1464: 1424: 1418: 1417: 1415: 1413: 1382: 1373: 1367: 1356: 1350: 1349: 1333: 1327: 1326: 1294: 1288: 1287: 1262:(3–4): 195–220. 1248: 1242: 1241: 1239: 1221: 1212: 1206: 1205: 1161: 1155: 1154: 1109: 1098: 1097: 1087: 1055: 1044: 1043: 1041: 1009: 988: 987: 985: 983: 956: 947: 938: 937: 935: 934: 924: 915: 914: 912: 911: 900: 891: 890: 888: 886: 859: 850: 849: 847: 846: 831: 717:, the long thin 662:transform faults 658:North Fiji Basin 611:Antarctic plates 541: 530: 522:Early Cretaceous 520:starting in the 501:starting in the 500: 494:between 570 and 486: 332:in the north to 327: 246:Philippine Plate 156: 149: 142: 135: 103:Australian Plate 92:Relative to the 46:Approximate area 31: 22:Australian Plate 19: 2514: 2513: 2509: 2508: 2507: 2505: 2504: 2503: 2484:Tectonic plates 2474: 2473: 2472: 2467: 2418: 2409: 2361: 2335:Reykjanes Ridge 2320:Knipovich Ridge 2265:Carlsberg Ridge 2246: 2163: 2069:North Galápagos 1890: 1802: 1793: 1762:Indo-Australian 1733: 1731:Tectonic plates 1728: 1698: 1697: 1661: 1660: 1656: 1624: 1619: 1618: 1614: 1607: 1592: 1591: 1587: 1577: 1575: 1554: 1549: 1548: 1544: 1508: 1507: 1503: 1473: 1472: 1468: 1426: 1425: 1421: 1411: 1409: 1399: 1380: 1375: 1374: 1370: 1357: 1353: 1335: 1334: 1330: 1296: 1295: 1291: 1250: 1249: 1245: 1219: 1214: 1213: 1209: 1163: 1162: 1158: 1121:(7419): 240–4. 1111: 1110: 1101: 1057: 1056: 1047: 1011: 1010: 991: 981: 979: 977: 954: 949: 948: 941: 932: 930: 926: 925: 918: 909: 907: 902: 901: 894: 884: 882: 880:10.1071/BT00023 861: 860: 853: 844: 842: 833: 832: 828: 823: 760: 736:Puysegur Trench 725:At the central 686:Niuafo'ou Plate 552: 536: 525: 505:(South African 495: 481: 448:plate tectonics 428: 422: 414:Capricorn Plate 379:biogeographical 368:Antarctic Plate 357:Macquarie Ridge 353:Puysegur Trench 322: 278: 254:Antarctic Plate 198: 151: 144: 137: 130: 17: 12: 11: 5: 2512: 2510: 2502: 2501: 2496: 2491: 2486: 2476: 2475: 2469: 2468: 2466: 2465: 2453: 2441: 2429: 2414: 2411: 2410: 2408: 2407: 2402: 2397: 2392: 2387: 2382: 2377: 2371: 2369: 2363: 2362: 2360: 2359: 2354: 2349: 2344: 2339: 2338: 2337: 2332: 2327: 2322: 2312: 2307: 2302: 2297: 2292: 2290:Explorer Ridge 2287: 2282: 2277: 2272: 2267: 2262: 2256: 2254: 2252:Oceanic ridges 2248: 2247: 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1303:Tectonophysics 1289: 1243: 1230:(1): 283–297. 1207: 1156: 1099: 1070:(2): 818–842. 1045: 989: 975: 939: 916: 892: 874:(3): 271–300. 851: 825: 824: 822: 819: 818: 817: 812: 807: 801: 796: 791: 786: 781: 776: 771: 766: 759: 756: 719:Kermadec Plate 698:Kermadec Plate 651:Torres Islands 635:Woodlark Basin 631:Woodlark Plate 596:Sumatra Trench 588:Eurasian Plate 551: 548: 524:between about 507:Kuunga Orogeny 455:Yilgarn Craton 444:Pilbara Craton 424:Main article: 421: 418: 390:Eurasian Plate 340:marked by the 277: 274: 272:microplates. 242:Eurasian Plate 197: 194: 113:and, largely, 107:tectonic plate 97: 96: 89: 88: 71: 67: 66: 63: 59: 58: 55: 51: 50: 47: 43: 42: 37: 33: 32: 24: 23: 15: 13: 10: 9: 6: 4: 3: 2: 2511: 2500: 2497: 2495: 2492: 2490: 2487: 2485: 2482: 2481: 2479: 2464: 2463: 2454: 2452: 2451: 2442: 2440: 2439: 2430: 2428: 2427: 2422: 2416: 2415: 2412: 2406: 2405:Phoenix Ridge 2403: 2401: 2398: 2396: 2393: 2391: 2388: 2386: 2383: 2381: 2378: 2376: 2373: 2372: 2370: 2368: 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1667: 1657: 1632: 1628: 1615: 1595: 1588: 1576:. Retrieved 1562: 1558: 1545: 1518: 1514: 1504: 1479: 1475: 1469: 1436: 1432: 1422: 1410:. Retrieved 1371: 1363: 1354: 1341: 1331: 1306: 1302: 1292: 1259: 1253: 1246: 1227: 1223: 1210: 1169: 1165: 1159: 1118: 1114: 1067: 1063: 1021: 1017: 980:. Retrieved 958: 931:. Retrieved 908:. Retrieved 883:. Retrieved 871: 867: 843:. Retrieved 839:the original 829: 815:Indian Plate 752: 740: 727:Alpine Fault 724: 655: 615: 600: 581: 577: 573: 565: 511: 489: 452: 429: 401:Indian Ocean 398: 382:Wallace line 376: 361: 346: 342:Alpine Fault 313: 309:North Island 279: 262:Indian Plate 230:Indian Ocean 199: 190:Indian Ocean 176:, including 166:Indian Ocean 164:beneath the 162:Indian Plate 159: 102: 100: 86:Indian Ocean 2380:Alpha Ridge 2375:Aegir Ridge 2330:Mohns Ridge 2305:Gorda Ridge 2280:Cocos Ridge 2275:Chile Ridge 2119:Solomon Sea 2059:North Andes 2049:Molucca Sea 1944:Conway Reef 1929:Bird's Head 1896:Microplates 1309:(1): 1–40. 1024:(1): 1–80. 982:26 December 804:Sunda Plate 731:New Zealand 715:Tonga Plate 702:New Zealand 690:Tonga Plate 592:Java Trench 584:Sunda Plate 394:Sunda Shelf 386:Australasia 370:called the 305:island arcs 218:New Zealand 210:Arafura Sea 204:, southern 186:New Zealand 105:is a major 82:New Zealand 2478:Categories 2260:Aden Ridge 2109:Seychelles 2024:Madagascar 1909:Aegean Sea 1866:Philippine 1767:Australian 1635:: 132–42. 933:2023-05-24 910:2015-12-25 845:2015-12-25 821:References 700:and on to 645:under the 533:Cenomanian 236:, and the 234:Tasman Sea 206:New Guinea 182:New Guinea 127:Antarctica 78:New Guinea 2149:Trobriand 2054:Niuafo’ou 2009:Kerguelen 1984:Halmahera 1979:Greenland 1964:Galápagos 1934:Capricorn 1924:Banda Sea 1914:Anatolian 1831:Caribbean 1752:Antarctic 1461:0025-3227 1439:: 69–84. 1412:24 August 1407:2201-702X 1284:0301-9268 1151:205230868 743:Antarctic 684:with the 682:Lau Basin 535:at about 518:Zealandia 503:Ediacaran 366:with the 320:Australia 316:Zealandia 284:with the 276:Geography 270:Macquarie 266:Capricorn 238:Timor Sea 214:Coral Sea 174:Australia 74:Australia 57:northeast 2450:Category 2242:Kshiroda 2227:Malvinas 2197:Farallon 2192:Cimmeria 2159:Woodlark 2154:Victoria 2114:Shetland 2014:Kermadec 1954:Explorer 1904:Adriatic 1836:Caroline 1757:Eurasian 1364:NY Times 1346:Archived 1224:Episodes 1194:23023129 1143:23023134 1094:52998637 758:See also 676:and the 562:devices. 544:Tasmania 514:Gondwana 492:Gondwana 426:Gondwana 374:(SEIR). 302:Kermadec 260:and the 188:and the 178:Tasmania 119:Gondwana 115:southern 70:Features 54:Movement 2462:Commons 2237:Phoenix 2212:Izanagi 2202:Insular 2187:Charcot 2104:Sangihe 2074:Okinawa 2044:Mariana 2029:Malpelo 2019:Lwandle 1994:Iranian 1989:Iberian 1886:Yangtze 1861:Okhotsk 1821:Arabian 1816:Amurian 1784:Pacific 1747:African 1676:Bibcode 1668:Geology 1637:Bibcode 1523:Bibcode 1484:Bibcode 1441:Bibcode 1311:Bibcode 1264:Bibcode 1202:4375902 1174:Bibcode 1123:Bibcode 1072:Bibcode 1026:Bibcode 747:heading 664:of the 641:of the 633:in the 478:Cratons 471:Yilgarn 467:Yilgarn 463:Pilbara 440:billion 420:Origins 192:basin. 111:eastern 109:in the 2177:Baltic 2099:Rovuma 2094:Rivera 2079:Panama 1969:Gonâve 1959:Futuna 1949:Easter 1876:Somali 1871:Scotia 1846:Indian 1772:Indian 1603:  1578:21 May 1459:  1405:  1395:  1282:  1200:  1192:  1166:Nature 1149:  1141:  1115:Nature 1092:  973:  885:21 May 475:Gawler 459:zircon 268:, and 256:, the 252:, the 248:, the 244:, the 232:, the 212:, the 208:, the 2222:Lhasa 2144:Tonga 2139:Tisza 2134:Timor 2084:Pelso 2039:Maoke 2034:Manus 1974:Gorda 1939:Coiba 1881:Sunda 1851:Nazca 1841:Cocos 1826:Burma 1625:(PDF) 1555:(PDF) 1381:(PDF) 1220:(PDF) 1198:S2CID 1147:S2CID 1090:S2CID 955:(PDF) 550:Speed 483:1,696 298:Tonga 290:Tonga 196:Scope 123:India 62:Speed 40:Major 2438:List 2217:Kula 1601:ISBN 1580:2023 1457:ISSN 1414:2024 1403:ISSN 1393:ISBN 1280:ISSN 1190:PMID 1139:PMID 984:2015 971:ISBN 887:2023 670:Fiji 469:and 457:and 300:and 292:and 226:Fiji 224:and 125:and 101:The 36:Type 2232:Moa 1684:doi 1645:doi 1633:478 1567:doi 1563:200 1531:doi 1492:doi 1449:doi 1437:347 1385:doi 1319:doi 1307:362 1272:doi 1260:118 1232:doi 1182:doi 1170:490 1131:doi 1119:490 1080:doi 1068:168 1034:doi 1022:181 963:doi 876:doi 729:in 668:to 560:GPS 527:132 509:). 497:530 450:. 157:. 132:100 2480:: 1682:. 1672:51 1670:. 1666:. 1643:. 1631:. 1627:. 1561:. 1557:. 1529:. 1519:23 1517:. 1513:. 1490:. 1480:66 1478:. 1455:. 1447:. 1435:. 1431:. 1401:. 1391:. 1344:. 1340:. 1317:. 1305:. 1301:. 1278:. 1270:. 1258:. 1228:35 1226:. 1222:. 1196:. 1188:. 1180:. 1168:. 1145:. 1137:. 1129:. 1117:. 1102:^ 1088:. 1078:. 1066:. 1062:. 1048:^ 1032:. 1020:. 1016:. 992:^ 969:. 957:. 942:^ 919:^ 895:^ 872:49 870:. 866:. 854:^ 598:. 538:96 416:. 396:. 359:. 344:. 324:85 311:. 220:, 184:, 153:60 146:45 139:96 84:, 80:, 76:, 1723:e 1716:t 1709:v 1692:. 1686:: 1678:: 1651:. 1647:: 1639:: 1609:. 1582:. 1569:: 1539:. 1533:: 1525:: 1498:. 1494:: 1486:: 1463:. 1451:: 1443:: 1416:. 1387:: 1366:. 1358:" 1325:. 1321:: 1313:: 1286:. 1274:: 1266:: 1240:. 1234:: 1204:. 1184:: 1176:: 1153:. 1133:: 1125:: 1096:. 1082:: 1074:: 1042:. 1036:: 1028:: 986:. 965:: 936:. 913:. 889:. 878:: 848:. 473:– 465:–

Index


Major
Australia
New Guinea
New Zealand
Indian Ocean
African Plate
tectonic plate
eastern
southern
Gondwana
India
Antarctica
100
96
45
60
Indian Plate
Indian Ocean
Indo-Australian Plate
Australia
Tasmania
New Guinea
New Zealand
Indian Ocean
Gulf of Carpentaria
New Guinea
Arafura Sea
Coral Sea
New Zealand

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