Assembly and break-up of Rodinia: Introduction to the special volume

Precambrian Research

Volumn 110, Issue 1-4, 2001, Pages 1-8

  Meert, J G ^a   Powell, C M A ^a  

^a Norwegian Geological Survey   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE; EDITORIAL; GEOLOGY; MAGNETISM;

EID: 0035420664     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0301-9268(01)00177-2     Document Type: Editorial

References (45)

1. Late Proterozoic extensional collapse in the Arabian-Nubian Shield
2. Breakup of a supercontinent between 625 and 555 Ma: New evidence and implications for continental histories
3. Laurentia-Siberia connection revisited
4. Pacific margins of Laurentia and East Antarctica-Australia as a conjugate rift pair: Evidence and implications for an Eocambrian supercontinent
5. On the organisation of American plates in the Neoprotertozoic and the breakout of Laurentia
6. Neoproterozoic-Paleozoic geography and tectonics: Review, hypothesis and environmental speculation
7. Laurentia-Kalahari collision and the assembly of Rodinia
8. Tibetan, Variscan and Precambrian basement reactivation: Products of continental collision
9. Integrated paleomagnetism and U-Pb geochronology of mafic dikes of the Eastern Anabar shield region, Siberia: Implications for Mesoproterozoic paleolatitude of Siberia and comparison with Laurentia
10. True polar wander, a supercontinental legacy
11. Stratigraphic, geochronological, and paleomagnetic constraints upon the Neoproterozoic climate paradox
12. A review of tectonic events in the East Antarctic Shield, and their implications for Gondwana and earlier supercontinents
13. Grenville-age basement provinces in East Antarctica: Evidence for three separate collisional orogens
14. Evidence for extensive Proterozoic remobilization of the Aldan shield and implications for Proterozoic plate tectonic reconstructions of Siberia and Laurentia
15. Paleomagnetic data and U-Pb isotopic age determinations from Coats Land, Antarctica: Implications for Neoproterozoic plate reconstructions
16. Was North America (Laurentia) part of southwestern Gondwanaland during the Late Proterozoic era
17. Plate tectonics: About turn for supercontinents
18. Did the breakout of Laurentia turn Gondwanaland inside-out?
19. The break-up of Rodinia, birth of Gondwana, true polar wander and the snowball earth
20. Continuation of the Mozambique Belt into East Antarctica: Grenville-age metamorphism and polyphase Pan-African high-grade events in central Dronning Maud Land
21. Refining Rodinia: Geologic evidence for the Australia-western US connection in the Proterozoic
22. Circum-Siberian Neoproterozoic ophiolite belt
23. Late Proterozoic low-latitude global glaciation: The snowball Earth
24. Evidence for a large-scale reorganization of Early Cambrian landmasses by inertial interchange true polar wander
25. New palaeomagnetic results from the 'cap dolomite' of the Neoproterozoic Walsh Tillite, northwestern Australia
26. A paleomagnetic analysis of Cambrian true polar wander
27. Growing Gondwana and rethinking Rodinia
28. The assembly of Gondwana 800-550 Ma
29. Southwest U.S.-East Antarctic (SWEAT) connection: A hypothesis
30. Stratigraphic evidence for the Siberia-Laurentia connection and Early Cambrian rifting
31. Palaeomagentic evidence for a Proterozoic supercontinent
32. The Neoproterozoic supercontinent: Rodinia or Palaeopangea?
33. Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?: Comment
34. Paleomagnetic constraints on timing of the Neoproterozoic breakup of Rodinia and the Cambrian formation of Gondwana
35. South Australian record of a Rodinian epicontinental basin and its mid-Neoproterozoic breakup (∼ 700 Ma) to form the Palaeo-Pacific Ocean
36. U-Pb geochronology of Riphean sandstone and gabbro from southeast Siberia and its bearing on the Laurentia-Siberia connection
37. New look at the Siberian connection: No SWEAT
38. Cambrian orogenic belt in East Antarctica and Sri Lanka: Implications for Gondwana assembly
39. Arc assembly and continental collision in the Neoproterozoic East African Orogen: Implications for the assembly of Gondwanaland
40. The reliability of paleomagnetic data
41. Geochronology and paleomagnetism of the Hunnedalen dykes, SW Norway: Implications for the Sveconorwegian apparent polar wander loop
42. The Proterozoic supercontinent Rodinia: Paleomagnetically derived reconstructions for 1100-1800 Ma
43. Age and paleomagnetism of the Mundine Well dyke swarm, Western Australia: Implications for an Australia-Laurentia connection at 750 Ma
44. Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?