B
Bryan Krapež
Researcher at Guilin University of Technology
Publications - 38
Citations - 2117
Bryan Krapež is an academic researcher from Guilin University of Technology. The author has contributed to research in topics: Banded iron formation & Volcanic rock. The author has an hindex of 20, co-authored 38 publications receiving 1744 citations. Previous affiliations of Bryan Krapež include Curtin University & University of Western Australia.
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Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic, and Biospheric Processes
Andrey Bekker,Bryan Krapež,John F. Slack,Noah J. Planavsky,Axel Hofmann,Kurt O. Konhauser,Olivier Rouxel +6 more
TL;DR: In this article, it was shown that occurrences of BIF, GIF, Pherozoic ironstones, and exhalites surrounding VMS systems are linked to diverse environmental changes.
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Relationship between detrital zircon age-spectra and the tectonic evolution of the Late Archaean Witwatersrand Basin, South Africa
Natalie Kositcin,Bryan Krapež +1 more
TL;DR: In this paper, detrital zircon geochronology can overcome the problem of overly quartzose compositions in Archaean sandstones due to severe chemical weathering and authigenic alteration, thereby enabling distinction between passive-margin and retroarc-basin stages through systematic changes in the age complexity of the source area.
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SHRIMP U-Pb zircon age constraints on the Late Archaean tectonostratigraphic architecture of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia
Natalie Kositcin,Stuart J.A. Brown,Mark Barley,Bryan Krapež,Kevin F. Cassidy,David C. Champion +5 more
TL;DR: In this paper, the Eastern Goldfields superterrane is assessed based on 35 new SHRIMP U-Pb zircon ages of supracrustal sequences.
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Physical volcanology and geochemistry of a Late Archaean volcanic arc: Kurnalpi and Gindalbie Terranes, Eastern Goldfields Superterrane, Western Australia
TL;DR: The Kurnalpi Terrane as mentioned in this paper contains calc-alkaline intermediate-silicic volcanic complexes, which were derived from large ion lithophile element (LILE) enriched mafic magmas by fractional crystallisation processes.
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Precipitation of iron silicate nanoparticles in early Precambrian oceans marks Earth's first iron age
TL;DR: The early ocean was characterized by anoxic, iron-rich (ferruginous) conditions before the rise of atmospheric oxygen ∼2.63-2.45 b.y..