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    U–Pb zircon geochronology of the eastern part of the Southern Ethiopian Shield by Stern, R., Ali, K., Abdelsalam, M., Wilde, Simon, Zhou, Q.

    Published 2012
    “…U–Pb zircon SHRIMP and LA-ICP-MS dating of 8 igneous and metamorphic intermediate and felsic bodies in the eastern SES yield Neoproterozoic crystallization ages: 847 ± 11, 855 ± 14, 732 ± 5, 665 ± 8, 657 ±6, 560 ± 8, and 548 ± 8 Ma. …”
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    U-Pb SHRIMP zircon geochronology and T-t-d history of the Kampa Dome, southern Tibet by Quigley, M., Liangjun, Y., Gregory, Courtney, Corvino, A., Sandiford, M., Wilson, C., Xiaohan, L.

    Published 2008
    “…Structural, petrographic and geochronologic studies of the Kampa Dome provide insights into the tectonothermal evolution of orogenic crust exposed in the North Himalayan gneiss domes of southern Tibet. U–Pb ion microprobe dating of zircons from granite gneiss exposed at the deepest levels within the dome yields concordia 206Pb/238U age populations of 506 ± 3 Ma and 527 ± 6 Ma, with no evidence of new zircon growth during Himalayan orogenesis. …”
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    SHRIMP U-Pb age constraints on magmatism and high-grade metamorphism in the Salem Block, southern India by Clark, Chris, Collins, Alan, Timms, Nicholas Eric, Kinny, Peter, Chetty, T., Santosh, M.

    Published 2009
    “…In this paper, we present Sensitive High Resolution Ion Microprobe (SHRIMP) U and Pb isotope analyses of zircon from a charnockite and a charnockite-hosted leucosome in order to determine the age of magmatism and anatexis related to high-grade metamorphism immediately to the north of the Palghat Cauvery Shear System (PCSS), a proposed Neoproterozoic terrane boundary within Southern India. …”
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    Detrital zircons in basement metasedimentary protoliths unveil the origins of southern India by Plavsa, Diana, Collins, A., Payne, J., Foden, J., Clark, Christopher, Santosh, M.

    Published 2014
    “…Coupled U-Pb and Hf isotopic analysis of detrital zircons from metasedimentary rocks of the Southern Granulite terrane (India) provides provenance information that helps unravel their paleotectonic position before Gondwana amalgamated. …”
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    SHRIMP U–Pb zircon geochronology of Neoproterozoic crustal granitoids (Southern Brazil): A case for discrimination of emplacement and inherited ages by da Silva, L., McNaughton, Neal, Fletcher, Ian

    Published 2005
    “…SHRIMP U–Pb zircon studies on two post-collisional granitic plutons and reassessment of the data previously reported for two anatectic gneissic granites are used to assess the late Neoproterozoic history of the Florianόpolis Batholith, southern Brazil. …”
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    Dating deposition and low-grade metamorphism by in situ U-Pb geochronology of titanite in the Paleoproterozoic Timeball Hill Formation, southern Africa by Rasmussen, Birger, Fletcher, Ian, Muhling, J.

    Published 2013
    “…The brown titanite is interpreted to be magmatic and to provide a reliable estimate for the age of deposition. In situ U--Pb dating of matrix-filling titanite cement from the same stratigraphic interval yields an age of 2145 ± 12 Ma, which corresponds with previous estimates for a low-grade tectonothermal event in southern Africa. …”
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    Age and origin of middle Neoproterozoic mafic magmatism in southern Yangtze Block and relevance to the break-up of Rodinia by Zhou, J., Li, X., Ge, W., Li, Zheng-Xiang

    Published 2007
    “…SHRIMP U–Pb zircon age, geochemical and Sm–Nd isotopic data are reported for mid-Neoproterozoic volcanic rocks and mafic intrusions in northern Guangxi (Guibei) and western Hunan (Xiangxi) Provinces along the southern margin of the Yangtze Block. …”
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    Untying the Kibaran knot: a reassessment of Mesoproterozoic correlations in southern Africa based on SHRIMP U-Pb data from the Irumide belt by De Waele, Bert, Wingate, Michael, Fitzsimons, Ian, Mapani, B.

    Published 2003
    “…The correlation between the Irumide belt and Choma-Kalomo block of southern Zambia has had a major influence on models for the tectonic assembly of southern Africa because it required that the intervening Neoproterozoic Zambezi belt was intracratonic and associated with minimal horizontal displacements. …”
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    Uncovering the Leichhardt Superbasin and Kalkadoon-Leichhardt Complex in the southern Mount Isa Terrane, Australia by Olierook, Hugo, Mervine, E.M., Armstrong, R., Duckworth, R., Evans, Noreen, McDonald, B., Kirkland, Chris, Shantha Kumara, A., Wood, D.G., Cristall, J., Jhala, K., Stirling, D.A., Friedman, I., McInnes, Brent

    Published 2022
    “…Here, we present zircon U-Pb and Hf isotopic data of granitoids, metabasalts and metasedimentary rocks from seven >1 km deep drill holes that provide a window into the basement geology of the southern parts of the Mount Isa Terrane. …”
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    Ion-probe dating of 1.2 Ga collision and crustal architecture in the Namaqua-Natal Province of southern Africa by Pettersson, A., Cornell, D., Moen, H., Reddy, Steven, Evans, D.

    Published 2007
    “…The Namaqua-Natal Province of southern Africa formed a part of the Kalahari craton, possibly linked to the ~1.0 Ga supercontinent Rodinia, but the timing of assembly and its positioning relation to other components is still debated. …”
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    Reconnaissance SHRIMP U–Pb zircon geochronology of the Tanzania Craton: Evidence for Neoarchean granitoid–greenstone belts in the Central Tanzania Region and the Southern East African Orogen by Kabete, J., McNaughton, Neal, Groves, D., Mruma, A.

    Published 2012
    “…Reconnaissance U–Pb sensitive high-resolution ion microprobe (SHRIMP) zircon dating of gneisses, granitoids and greenstones from well-documented study areas within the Tanzania Craton indicates that: (1) ~2815–2691 Ma greenschist-amphibolite facies greenstones and associated granitoids are confined within extensive >3600 Ma granitoid–gneisses in the Central Tanzania Region; (2) greenschist-amphibolite facies greenstone rocks from the Singida-Mayamaya Terrane in the south-eastern Lake Nyanza Superterrane, Lake Victoria Region are older than 2681 Ma; (3) greenschist to lower-granulite facies granitoid–greenstone belts from the Kilindi-Handeni Superterrane, within the largely Neoproterozoic Southern East African Orogen are older than 2670 Ma; and (4) the granitoid–greenstone belts within the Dodoma Basement Superterrane, Central Tanzania Region and Kilindi-Handeni Superterrane, Southern East African Orogen are broadly coeval with ~2823–2671 Ma granitoid–greenstone belts in the Lake Nyanza Superterrane, in the Lake Victoria Region. …”
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    The Chiquerío Formation, southern Peru by Chew, D., Kirkland, Chris

    Published 2011
    “…The Chiquerío Formation (Fm.) is a thick glaciogenic succession deposited unconformably on gneisses of the Arequipa massif in southern Peru. It has undergone greenschist facies metamorphism during Early Palaeozoic orogenesis. …”
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