Structural and geochronological constraints on the evolution of the eastern margin of the Tanzania Craton in the Mpwapwa area, central Tanzania

[1]  N. Boniface,et al.  Neoproterozoic eclogites in the Paleoproterozoic Ubendian Belt of Tanzania: Evidence for a Pan-African suture between the Bangweulu Block and the Tanzania Craton , 2012 .

[2]  P. Vermeesch.  On the visualisation of detrital age distributions , 2012 .

[3]  Y. Amelin,et al.  A new geological framework for south-central Madagascar, and its relevance to the “out-of-Africa” hypothesis , 2011 .

[4]  R. Thomas,et al.  The Mecubúri and Alto Benfica Groups, NE Mozambique: Aids to unravelling ca. 1 and 0.5Ga events in the East African Orogen , 2010 .

[5]  R. Key,et al.  Post-collisional magmatism in the central East African Orogen: The Maevarano Suite of north Madagascar , 2010 .

[6]  H. Fritz,et al.  Hot granulite nappes — Tectonic styles and thermal evolution of the Proterozoic granulite belts in East Africa , 2009 .

[7]  R. Thomas,et al.  Geochronology of the Precambrian crust in the Mozambique belt in NE Mozambique, and implications for Gondwana assembly , 2009 .

[8]  A. Kröner,et al.  Isothermal decompression history in the “Western Granulite” terrain, central Tanzania: Evidence from reaction textures and trapped fluids in metapelites , 2008 .

[9]  D. Cozzupoli,et al.  Compressional reworking of the East African Orogen in the Uluguru Mountains of eastern Tanzania at c. 550 Ma: implications for the final assembly of Gondwana , 2008 .

[10]  Y. Motoyoshi,et al.  Geodynamic Evolution of East Antarctica: A Key to the East–West Gondwana Connection , 2008 .

[11]  R. Thomas,et al.  Early Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orogen? , 2008 .

[12]  S. Johnson,et al.  Protolith Ages and Timing of Metasomatism Related to the Formation of Whiteschists at Mautia Hill, Tanzania: Implications for the Assembly of Gondwana , 2006, The Journal of Geology.

[13]  M. Wingate,et al.  Archaean and Palaeoproterozoic gneisses reworked during a Neoproterozoic (Pan-African) high-grade event in the Mozambique belt of East Africa: Structural relationships and zircon ages from the Kidatu area, central Tanzania , 2006 .

[14]  A. Kröner,et al.  Reworking of Archaean and Palaeoproterozoic crust in the Mozambique belt of central Tanzania as documented by SHRIMP zircon geochronology , 2005 .

[15]  S. Pisarevsky,et al.  Amalgamating eastern Gondwana: The evolution of the Circum-Indian Orogens , 2005 .

[16]  R. Thomas,et al.  Himalayan-type indenter-escape tectonics model for the southern part of the late Neoproterozoic–early Paleozoic East African– Antarctic orogen , 2004 .

[17]  S. Reddy,et al.  Temporal constraints on Palaeoproterozoic eclogite formation and exhumation (Usagaran Orogen, Tanzania) , 2004 .

[18]  S. Reddy,et al.  Heterogeneous excess argon and Neoproterozoic heating in the Usagaran Orogen, Tanzania, revealed by single grain 40Ar/39Ar thermochronology , 2004 .

[19]  S. Muhongo,et al.  Neoarchaean magmatism and metamorphism of the western granulites in the central domain of the Mozambique belt, Tanzania: U–Pb shrimp geochronology and PT estimates , 2003 .

[20]  S. Reddy,et al.  Complex high-strain Deformation in the Usagaran Orogen, Tanzania:Structural Setting of Palaeoproterozoic Eclogites , 2003 .

[21]  M. Wingate,et al.  Single-zircon geochronology and Nd isotopic systematics of Proterozoic high-grade rocks from the Mozambique belt of southern Tanzania (Masasi area): implications for Gondwana assembly , 2003, Journal of the Geological Society.

[22]  A. Kröner,et al.  Single Zircon Evaporation and SHRIMP Ages for Granulite‐Facies Rocks in the Mozambique Belt of Tanzania , 2001, The Journal of Geology.

[23]  K. Mezger,et al.  U-Pb dating of metamorphic minerals: Pan-African metamorphism and prolonged slow cooling of high pressure granulites in Tanzania, East Africa , 2000 .

[24]  M. A. Maboko.  Nd and Sr isotopic investigation of the Archean–Proterozoic boundary in north eastern Tanzania: constraints on the nature of Neoproterozoic tectonism in the Mozambique Belt , 2000 .

[25]  A. Boven.  Timing of exhumation of a high-pressure mafic granulite terrane of the Paleoproterozoic Ubende belt (West Tanzania) , 1999 .

[26]  K. Mezger,et al.  Evidence for a 2 Ga subduction zone: Eclogites in the Usagaran belt of Tanzania , 1995 .

[27]  A. Mruma.  Stratigraphy and palaeodepositional environment of the Palaeoproterozoic volcano-sedimentary Konse Group in Tanzania , 1995 .

[28]  J. Lenoir,et al.  The Palaeoproterozoic Ubendian shear belt in Tanzania: geochronology and structure , 1994 .

[29]  R. Stern.  ARC Assembly and Continental Collision in the Neoproterozoic East African Orogen: Implications for the Consolidation of Gondwanaland , 1994 .

[30]  E. Verdurmen,et al.  Possible zircon UPb evidence for Pan-African granulite-facies metamorphism in the Mozambique belt of southern Tanzania , 1982 .

[31]  J. Hepworth.  The Mozambique orogenic belt and its foreland in northeast Tanzania: a photogeologically-based study , 1972, Journal of the Geological Society.