Late neoproterozoic assembly of East Gondwana

Geology

Volumn 30, Issue 1, 2002, Pages 3-6

  Powell, C McA ^a   Pisarevsky, S A ^a  

^a UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

Author keywords

Australia; Gondwana; India; Neoproterozoic; Paleomagnetism

Indexed keywords

AMALGAMATION;

GEOCHRONOLOGY; GEOGRAPHICAL REGIONS; MAGNETISM;

GEOLOGY;

CONTINENTAL BREAKUP; GONDWANA; PALEOMAGNETISM; PROTEROZOIC; RODINIA; SUPERCONTINENT;

AUSTRALIA; INDIA;

EID: 84879879830     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2002)030<0003:LNAOEG>2.0.CO;2     Document Type: Article

References (37)

1. Assembling West Gondwana in the Neoproterozoic: Clues from the São Francisco craton region, Brazil
2. U-Pb chronology of the Northampton Complex, Western Australia-Evidence for Grenvillian sedimentation, metamorphism and deformation and geodynamic implications
3. Neoproterozoic-Paleozoic geography and tectonics: Review, hypothesis, environmental speculation
4. The Malagarazi supergroup of SE Burundi and its correlative Bukoba Supergroup of NW Tanzania: Neo- and Mesoproterozoic chronostratigraphic constraints from Ar-Ar ages on mafic intrusive rocks
5. Low paleolatitude of deposition for Late Precambrian periglacial varvites in South Australia: Implications for paleoclimatology
6. Stratigraphic, geochronological, and paleomagnetic constraints upon the Neoproterozoic climatic paradox
7. A high-quality mid-Neoproterozoic paleomagnetic pole from South China, with implications for ice ages and the breakup configuration of Rodinia
8. Grenville-age basement provinces in East Antarctica: Evidence for three separate collisional orogens
9. Neoproterozoic sinistral displacement along the Darling mobile belt, Western Australia, during Gondwanaland assembly
10. Continuation of the Mozambique belt into East Antarctica: Grenville-age metamorphism and polyphase Pan-African high-grade events in central Dronning Maude Land
11. The Precambrian-Cambrian boundary problem: Paleomagnetic directions from the Amadeus basin, central Australia
12. South China in Rodinia: Part of the missing link between Australia-East Antarctica and Laurentia?
13. The breakup of Rodinia: Did it start with a mantle plume beneath South China?
14. Palaeomagnetism of some rocks from Peninsular India and Kashmir
15. Late Precambrian paleomagnetism in Australia: The Adelaide geosyncline
16. The assembly of Gondwana 800-550 Ma
17. Paleomagnetic investigation of the Late Proterozoic Gagwe lavas and Mbozi complex, Tanzania, and the assembly of Gondwana
18. 39Ar dating of metamorphic and magmatic minerals: Implications for the SWEAT correlation
19. Chronology and evolution of Middle Proterozoic Albany-Fraser orogen, Western Australia
20. A palaeomagnetic study of Empress 1A, a stratigraphic drillhole in the Officer basin: New evidence for the low-latitude position of Australia in the Neoproterozoic
21. Reconstructions of the Panthalassan margin of Gondwanland
22. Paleomagnetic constraints on timing of the Neoproterozoic breakup of Rodinia and the Cambrian formation of Gondwana
23. South Australian record of a Rodinian epicontinental basin and its mid-Neoproterozoic breakup (∼700 Ma) to form the Palaeo-Pacific Ocean
24. Palaeomagnetic constraints on the position of the Kalahari craton in Rodinia
25. Late Precambrian (850-800 Ma) palaeomagnetic pole for the South Indian shield from the Harohalli alkaline dykes: Geotectonic implications for Gondwana reconstructions
26. The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia
27. Low palaeolatitude of Late Proterozoic glaciation: Early timing of remanence in haematite of the Elatina Formation, South Australia
28. Paleomagnetic polarity reversals in Marinoan (ca. 600 Ma) glacial deposits of Australia: Implications for the duration of low-latitude glaciation in Neoproterozoic time
29. Arc assembly and continental collision in the Neoproterozoic East African Orogen: Implications for the assembly of Gondwanaland
30. Palaeomagnetic and petrological reconstruction of the Seychelles
31. Rodinia refined or obscured: Palaeomagnetism of the Malani Igneous Suite (NW India)
32. Geochronology and paleomagnetism of the Seychelles microcontinent: The India link
33. The reliability of paleomagnetic data
34. The Proterozoic supercontinent Rodinia: Paleomagnetically derived reconstruction for 1100 to 800 Ma
35. The nature and origin of Late Proterozoic high-grade gneisses of the Leeuwin block, Western Australia
36. Age and palaeomagnetism of the Mundine Well dyke swarm, Western Australia: Implications for an Australia-Laurentia connection at 755 Ma