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滹沱群青石村组古风化壳的形成环境 被引量:1

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作者 张翊钧
出处 《山西地质》 1990年第3期260-266,共7页
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  • 1钟华,马永生.五台山滹沱群早元古代白云岩氧同位素地球化学研究[J].地球化学,1995,24(C00):83-91. 被引量:3
  • 2储雪蕾.新元古代的“雪球地球”[J].矿物岩石地球化学通报,2004,23(3):233-238. 被引量:33
  • 3钟华,马永生.早元古代碳同位素突变的发现[J].地质学报,1995,69(2):185-191. 被引量:4
  • 4Pavlov A A, Kasting J F. Mass-independet fractionation of sulfer isotope in Archean sediments: Strong evidence for an anoxic Archean atmosphere. Astrobiology, 2002, 2:27-41.
  • 5Kirschvink J L, Gaidos E J, Bertani L E. Paleoproterozoic snowball Earth: Extreme climatic and geochemical global change and its bio- logical consequences. Proc Natl Acad Sci USA, 2000, 97:1400-1405.
  • 6Evans D A, Beukes N J, Kirschvink J L. Low-latitude glaciation in the Palaeoproterozoic era. Nature, 1997, 386:262-266.
  • 7Kopp R E, Kirschvink J L, Hilburn I A, et al. The paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxy genic photosyntheis. Proc Natl Acad Sci USA, 2005, 102:11131-11136.
  • 8Barley M E, Bekker A, Krapez B. Late Archean to Early Paleoproterozoic global tectonics, environmental change and the rise of atmos- pheric oxygen. Earth Planet Sci Lett, 2005, 238:156-171.
  • 9Hayes J M. Global methanotrophy at the Archean-Proterozoic transition. In: Bengston S, ed. Early Life on Earth. Vol 84. New York: Co- lumbia University Press, 1994. 220-236.
  • 10Pavlov A A, Kasting J F, Brown L L. Greenhouse warming by CH4 in the atmosphere of early Earth. J Geophys Res, 2000, 105: 11981-11990.

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