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English: Paleotectonic map of eastern Gondwana with the Pan-African and/or circum-Antarctic orogenic (“mobile”) belts highlighted by age differences (See Fitzsimons, 2000a, cited in Meert, 2003, see source data below). Meaning of abbreviations: Af = Afif terrane (Saudi Arabia); AFB = Albany-Fraser Belt (Australia); AS = Angavo shear zone (Madagascar); BH = Bunger Hills (Antarctica); BR = Bongolava-Ranotsara shear zone (Madagascar); BS = Betsimisaraka suture zone (Madagascar); DB = Damara Belt (Africa); DDS = Darling-Denman suture (Antarctica - Australia); DG = Denman Glacier (Antarctica); DMS = Dronning Maud suture (Antarctica); EG = Eastern Ghats (India); GB = Gariep Belt (Africa); HC = Highland Complex (Sri Lanka); LA = Lufilian Arc (Africa); LG = Lambert Graben (Antarctica); LHB = Lützow-Holm Belt (Antarctica); MD = Mwembeshi Dislocation (Africa); MP = Maud Province (Antarctica); NBS = Nabitah Suture (Arabia); nPCSM = Northern Prince Charles Mountains (Antarctica); NQ = Namaqua Belt (Africa); OSH = Onib-Sol Hamed suture (Arabia); PBB = Prydz Bay Belt (Antarctica); PC = Paughat-Cauvery (India); SB = Saldania Belt (Africa); SR = Shackelton Range (Antarctica) ; UAA = Urd Al Amar suture (Arabia); VC = Vijayan Complex (Sri Lanka); WC = Wanni Complex (Sri Lanka); WI = Windmill Islands (Antarctica); ZB = Zambezi Belt (Africa).
Datum 6. mart 2006. (izvorni datum postavljanja)
Izvor Adapted from fig 2 in: Joseph G. Meert (2003): A synopsis of events related to the assembly of eastern Gondwana. Tectonophysics 362(1–4; Special Issue Paleomagnetism Applied to Tectonics. A tribute to Rob Van der Voo.):1–40, doi:10.1016/S0040-1951(02)00629-7 (manuscript available at UFL). The editor is the author of the above paper and has modified the figure included in the paper.
Originally uploaded to the English Wikipedia by Jmeert.
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  • 2006-03-06 14:15 Jmeert 1000×785×8 (220296 bytes) http://www.clas.ufl.edu/users/jmeert/kuunga.jpg adapted from: Meert, J.G., A synopsis of events related to the assembly of eastern Gondwana, Tectonophysics, 362, 1-40 The editor is the author of the above paper and has modified the figure included in t

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