Titlebook: Reading the Archive of Earth’s Oxygenation; Volume 1: The Palaeo Victor A. Melezhik,Anthony R. Prave,Eero J. Hanski Book 2013 Springer-Verl

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4.2 The Pechenga Greenstone Beltreenstone Belt. In an attempt to resolve the terminology, Melezhik (1996) suggested the name Transfennoscandian Greenstone Belt (Fig. 3.1); however, it remains to be seen whether or not this will be used in practice.

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3.3 Palaeotectonic and Palaeogeographic Evolution of Fennoscandia in the Early Palaeoproterozoicorogenies. Figure 3.22 provides a general guide through the tectonic and associated palaeogeographic stages and Figs. 3.23, 3.24, 3.25, 3.26, 3.27, 3.28, and 3.29 illustrate the main rock types representing the salient features of the early Palaeoproterozoic evolution of the Fennoscandian Shield.

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3.2 Litho- and Chronostratigraphy of the Palaeoproterozoic Karelian Formationsoses and commonly lack precise geochronological control. This has hampered the development of robust chronostratigraphic frameworks for such successions, and restricted reconstruction of their geological histories. It has also led to the proliferation of many local stratigraphic nomenclatures rife with numerous formal and informal names.

摘要

1.1 Tectonic Evolution and Major Global Earth-Surface Palaeoenvironmental Events in the Palaeoproterlay of plate tectonics and deep mantle dynamics resulting in supercontinental cycles and (super)plume events (Condie et al. 2001; Condie 2004). These processes include the amalgamation, dispersal, collision and geographic position of major land-masses which dictate volcanic and hydrothermal activiti

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2.1 The International Continental Scientific Drilling Programontinuous rock sections through key geological formations which are not accessible by any other means but crucial for understanding Earth’s surface processes and their evolution, and providing direct information on processes operating at depth. ICDP has overseen 15 years of successful coordination o

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3.2 Litho- and Chronostratigraphy of the Palaeoproterozoic Karelian Formationsted by abundant high-precision radiometric dates. In contrast, Precambrian metasedimentary successions contain few fossils useful for correlation purposes and commonly lack precise geochronological control. This has hampered the development of robust chronostratigraphic frameworks for such successio