Search Results - "Augland, L."
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The main pulse of the Siberian Traps expanded in size and composition
Published in Scientific reports (10-12-2019)“…Emplacement of large volumes of (sub)volcanic rocks during the main pulse of the Siberian Traps occurred within <1 m.y., coinciding with the end-Permian mass…”
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High-precision UPb zircon dating of explosive volcanism in an early bi-modal volcano-sedimentary sequence from the Isle of Mull, North Atlantic Igneous Province
Published in Lithos (01-10-2024)“…The North Atlantic Igneous Province (NAIP) forms one of the best studied Large Igneous Provinces (LIP) on the planet, however, significant uncertainties…”
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The first CA-ID-TIMS U-Pb dating of the Tithonian/Berriasian boundary beds in a Boreal succession
Published in Gondwana research (01-06-2023)“…[Display omitted] •The first high-precise numerical age for Tithonian/Berriasian boundary in Arctic.•Tuff layers dated by high-resolution…”
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Ordovician shoshonitic to ultrapotassic volcanism in the central Norwegian Caledonides: The result of sediment subduction, mantle metasomatism and mantle partial melting
Published in Lithos (01-03-2020)“…Shoshonitic to ultrapotassic, mantle-derived volcanic rocks found within certain accretionary and collisional settings have trace element patterns comparable…”
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A new high-resolution stratigraphic and palaeoenvironmental record spanning the End-Permian Mass Extinction and its aftermath in central Spitsbergen, Svalbard
Published in Palaeogeography, palaeoclimatology, palaeoecology (15-09-2020)“…Research on the Permian-Triassic boundary (PTB) along the northern margins of Pangaea (exposed today in the Arctic region) has been heavily reliant on field…”
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The Heggmovatn supracrustals, North Norway—A late Mesoproterozoic to early Neoproterozoic (1050–930Ma) terrane of Laurentian origin in the Scandinavian Caledonides
Published in Precambrian research (01-08-2012)“…[Display omitted] ► The Heggmo rocks previously thought to represent Baltic basement of ca. 1.8Ga. ► We report U–Pb zircon data on clastic and magmatic zircons…”
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Structural constraints on the evolution of the Meatiq Gneiss Dome (Egypt), East-African Orogen
Published in Journal of African earth sciences (1994) (01-07-2010)“…Amphibolite-grade quartzofeldspathic gneiss domes surrounded by greenschist-grade island arc and ophiolitic assemblages is a characteristic feature of the…”
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