Results 51 to 60 of about 32,456 (106)
The initial break-up of Pangæa elicited by Late Palæozoic deglaciation. [PDF]
Yeh MW, Shellnutt JG.
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Mapping a hidden terrane boundary in the mantle lithosphere with lamprophyres. [PDF]
Dijkstra AH, Hatch C.
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Pre-Variscan evolution of the Western Tatra Mountains: new insights from U-Pb zircon dating. [PDF]
Burda J, Klötzli U.
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Enhanced erosion by continental arc volcanism as a driver of the Cambrian Explosion. [PDF]
Wu Y +12 more
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U-Pb dating of volcaniclastic deposits from the Sinj Basin: implications for provenance and the tectono-sedimentary evolution of the External Dinarides. [PDF]
Šamarija R +6 more
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High-K magmatism of the central Urumieh-Dokhtar magmatic arc (UDMA) documents the final stages of NeoTethyan Ocean subduction. The temporal and spatial development of collision-related magmatism in this region remains ambiguous because of the paucity of ...
Choi, Sung Hi +5 more
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The Strona-Ceneri Zone comprises the deformed and metamorphosed remains of a Late Proterozoic or Paleozoic subduction-accretion complex that was intruded by Ordovician granitoids.
Zurbriggen, R., Handy, M. R., Franz, L.
core
A novel sample pre-screening methodology for accurate in situ U-Pb dating of zircon crystals. [PDF]
Kis A.
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Des études géochronologiques U-Pb et géochimiques (éléments majeurs, traces et terres rares) ont été effectuées sur différentes formations ortho- et paradérivées du Sud-Est du Massif Central (France). Les granites du Mendic et des Palanges, témoins directs du magmatisme cadomien, sont respectivement datés à 603 ± 9 Ma et 540 ± 18 Ma.
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