Zobrazeno 1 - 10
of 280
pro vyhledávání: '"H. U. Schmincke"'
Autor:
M. Sacchi, G. De Natale, V. Spiess, L. Steinmann, V. Acocella, M. Corradino, S. de Silva, A. Fedele, L. Fedele, N. Geshi, C. Kilburn, D. Insinga, M.-J. Jurado, F. Molisso, P. Petrosino, S. Passaro, F. Pepe, S. Porfido, C. Scarpati, H.-U. Schmincke, R. Somma, M. Sumita, S. Tamburrino, C. Troise, M. Vallefuoco, G. Ventura
Publikováno v:
Scientific Drilling, Vol 26, Pp 29-46 (2019)
Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large
Externí odkaz:
https://doaj.org/article/5212840a879842549100d10d12380aae
Autor:
T. Litt, F. S. Anselmetti, H. Baumgarten, J. Beer, N. Cagatay, D. Cukur, E. Damci, C. Glombitza, G. Haug, G. Heumann, H. Kallmeyer, R. Kipfer, S. Krastel, O. Kwiecien, A. F. Meydan, S. Orcen, N. Pickarski, M.-E. Randlett, H.-U. Schmincke, C. J. Schubert, M. Sturm, M. Sumita, M. Stockhecke, Y. Tomonaga, L. Vigliotti, T. Wonik, the PALEOVAN Scientific Team
Publikováno v:
Scientific Drilling, Vol 14, Pp 18-29 (2012)
International Continental Scientific Drilling Program (ICDP) drilled a complete succession of the lacustrine sediment sequence deposited during the last ~500,000 years in Lake Van, Eastern Anatolia (Turkey). Based on a detailed seismic site survey, t
Externí odkaz:
https://doaj.org/article/84414487ddd54cd697419cf1180d4bc2
Akademický článek
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Publikováno v:
Geo-Marine Letters. 20:160-167
Detailed morphological data collected from the submarine flanks of the Canary Islands have revealed numerous submarine canyons down to water depths of >3,000 m. These canyons are interpreted to have formed by submarine erosion. We postulate formation
Autor:
E. Harms, H. U. Schmincke
Publikováno v:
Contributions to Mineralogy and Petrology. 138:84-98
A volatile-rich and chemically zoned phonolitic magma reservoir was tapped successively during the eruption of Laacher See volcano ca. 12,900 years BP and produced a tephra sequence consisting of phenocryst-poor, highly evolved phonolite at the base
Publikováno v:
Journal of Volcanology and Geothermal Research. 92:215-229
To constrain life time and flow rates in a submarine lava tube (pillow), 3D finite-element calculations were carried out for a simplified fixed geometry model tube. The principal parameters included into the model are: a temperature-dependent Newtoni
Publikováno v:
Eiszeitalter und Gegenwart, Vol 39, Pp 62-86 (1989)
Die quartäre Sedimentfolge der Kärlicher Tongrube ist ein Schlüsselprofil für das Pleistozän Mitteleuropas: (a) Rhein- und Mosel-Terrassenablagerungen belegen die junge tektonische Hebung des paläozoischen Rheinischen Schildes, (b) Löß- und P
Externí odkaz:
https://doaj.org/article/d0772a3c17a840b49eed9d8811396ec4
Autor:
H. U. Schmincke, Susanne M. Straub
Publikováno v:
Geologische Rundschau. 87:461-476
We studied the volcanic contribution to the global sediment budget in the Pacific Ocean basin. It is the world's oldest (174 m.y.) and largest (≈49% of Earth's surface area) ocean basin and has had a high and continuous tephra influx from intraplat
Lake Formation and Catastrophic Dam Burst during the Late Pleistocene Laacher See Eruption (Germany)
Autor:
H.-U. Schmincke, C. Park
Publikováno v:
Naturwissenschaften. 84:521-525
and rising more than 15m above the pre-eruptive land surface. Collapse of the unstable dam prior to the final phase of the eruption resulted in sudden drainage of the lake. Deposits laid down by the catastrophic floodwaves occur at least as far north
Publikováno v:
Geologische Rundschau. 86:637-669
The Late Miocene to Pleistocene evolution of the northwestern Iblean plateau (Sicily) is marked by a complex interplay of subaerial and submarine volcanism, subsidence and uplift, eustatic sea-level changes, and shallow-water carbonate and clay sedim