Zobrazeno 1 - 10
of 223
pro vyhledávání: '"Miogeocline"'
Autor:
B. S. Petrushkov, A. V. Gavrish, N. S. Bortnikov, A. A. Bagaeva, Galina A. Palyanova, V. F. Proskurnin
Publikováno v:
Doklady Earth Sciences. 484:12-17
The variety of sizes and morphology of grains and chemical composition of native Au, and the diversity of mineral productive associations in the new ore occurrences of the Western and Central Taimyr (the Minina–Bolshevik miogeocline and the Shrenk
Akademický článek
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Publikováno v:
Canadian Journal of Earth Sciences. 53:140-155
Triassic rocks of the Western Canada Sedimentary Basin (WCSB) have previously been interpreted as being deposited on the passive margin of North America. Recent detrital zircon provenance studies on equivalent Triassic rocks in the Yukon have suggest
Publikováno v:
Geosphere. 10:1402-1410
U-Pb detrital zircon geochronology provides insight into the provenance of the upper Neoproterozoic–lower Cambrian Osgood Mountain Quartzite and the upper Cambrian–lower Ordovician Preble Formation in the Osgood Mountains of northern Nevada (USA)
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Publikováno v:
Lithosphere. 5:17-28
Coupled U-Pb ages and Hf isotopic ratios in zircons from Proterozoic basement and three siliciclastic cover sequences in southern California provide important insights into the formation of the southern Mojave crustal province and its incorporation i
Autor:
Charles A. Ferguson
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
George E. Gehrels, Andrew Leier
Publikováno v:
Geology. 39:399-402
Lower Cretaceous strata and the underlying sub-Cretaceous unconformity in western North America record a profound, but poorly understood change in sedimentation patterns and basin dynamics in the Cordilleran foreland basin. To better understand the r
Publikováno v:
Geological Society of America Bulletin. 123:1539-1559
Current understanding of secular changes in the carbon isotopic composition of mid- to late Ediacaran carbonates suggests a relatively long, steady recovery of the global ocean from the Shuram negative excursion, followed by a smaller negative excurs
Autor:
Martin J. Kennedy, David Mrofka
Publikováno v:
Geological Society, London, Memoirs. 36:449-458
The late Neoproterozoic Kingston Peak Formation (Fm.) is a several-kilometre-thick sedimentary succession primarily influenced by syndepositional tectonism and located in the region around Death Valley, California (Fig. 40.1). Its distribution is div