Petrogenesis and tectonic significance of the Baipu granite porphyry in the Huangtian uranium deposit, northeastern Guangdong, South China. [PDF]
Ruan K, Wu J, Long Z, Min Z.
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Impact-induced initiation of Snowball Earth: A model study. [PDF]
Fu M, Abbot DS, Koeberl C, Fedorov A.
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Petrographic and geochemical study of Precambrian and Paleozoic rocks in the western Anti-Atlas belt, Morocco: Facies, weathering, provenance and economic exploitation. [PDF]
Sebbab MM +10 more
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Devonian northward drift of the Qaidam-Kunlun continent constrains the early evolution of the Paleo-Tethys Ocean. [PDF]
Song P +6 more
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Strong nickel enrichment co-located with redox-organic interactions in Neretva Vallis, Mars. [PDF]
Manelski HT +18 more
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Paleoproterozoic molassoid complexes of Central Karelia
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Breakup of a Paleoproterozoic Supercontinent
Gondwana Research, 2002Abstract If a Paleoproterozoic supercontinent broke up between 1.6 and 1.5 Ga, the distribution of sutures shows that the breakup was not complete. At least two large cratons, Atlantica (Amazonia, Congo, West Africa and probably North Africa and Rio de la Plata) and Arctica (Laurentia, Siberia, Baltica, North Australia and North China), survived the ...
Kent C Condie
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Abstract We document for the first time the presence of a Paleoproterozoic ophiolitic melange in the Archean–Paleoproterozoic Kongling Complex in the northern Huangling Dome, Yangtze craton, South China. Detailed field mapping, petrographic, geochronological and geochemical studies reveal that the melange consists of a suite of amphibolite facies ...
Qingsen Han +2 more
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Archean-Paleoproterozoic transition: The Indian perspective
Earth-Science Reviews, 2019Abstract India has perhaps the richest Paleoarchean to Paleoproterozoic crustal components on Earth ( Miller et al., 2018 ). Notwithstanding this, much of the Indian subcontinent remains unexplored compared to other ancient cratons in North America, Australia, Brazil and Africa.
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A Paleoproterozoic A-type Rhyolite
Chinese Journal of Geochemistry, 1999The rhyolites in the upper Luliang Group of Shanxi, China, are Paleoproterozoic weakly alkaline volcanic rocks. They are characterized by high SiO2, Na2O + K2O, Zr, Nb, Ga, Y and REE contents and large FeO* /MgO, Rb/Sr and Ga/Al ratios, and low CaO, Sr and Eu contents, and share much in common with the A-type granitic rocks.
Yu Jinhai, Wang Dezi
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