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  • 1
    Monograph available for loan
    Monograph available for loan
    Chichester [u.a.] : Wiley
    Call number: M 98.0493
    Type of Medium: Monograph available for loan
    Pages: xii, 534 S.
    Edition: 3rd ed.
    ISBN: 047196543X
    Classification:
    C.2.4.
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: M 96.0420
    Type of Medium: Monograph available for loan
    Pages: XI, 432 S.
    ISBN: 9054105100
    Classification:
    Mathematical Geology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Keywords: volcanism ; volcanic systems ; small-scale volcanoes
    Description / Table of Contents: I. E. M. Smith and K. Németh: Source to surface model of monogenetic volcanism: a critical review / Geological Society, London, Special Publications, 446:1-28, first published on March 31, 2017, doi:10.1144/SP446.14 --- Volker Lorenz, Peter Suhr, and Stefan Suhr: Phreatomagmatic maar-diatreme volcanoes and their incremental growth: a model / Geological Society, London, Special Publications, 446:29-59, first published on September 27, 2016, doi:10.1144/SP446.4 --- Karen G. Bemis and Margot Ferencz: Morphometric analysis of scoria cones: the potential for inferring process from shape / Geological Society, London, Special Publications, 446:61-100, first published on January 17, 2017, doi:10.1144/SP446.9 --- Stephan Kurszlaukis and Volker Lorenz: Differences and similarities between emplacement models of kimberlite and basaltic maar-diatreme volcanoes / Geological Society, London, Special Publications, 446:101-122, first published on October 5, 2016, doi:10.1144/SP446.5 --- R. A. F. Cas, J. van Otterloo, T. N. Blaikie, and J. van den Hove: The dynamics of a very large intra-plate continental basaltic volcanic province, the Newer Volcanics Province, SE Australia, and implications for other provinces / Geological Society, London, Special Publications, 446:123-172, first published on November 7, 2016, doi:10.1144/SP446.8 --- H. Murcia, J. M. Lindsay, K. Németh, I. E. M. Smith, S. J. Cronin, M. R. H. Moufti, N. N. El-Masry, and S. Niedermann: Geology and geochemistry of Late Quaternary volcanism in northern Harrat Rahat, Kingdom of Saudi Arabia: implications for eruption dynamics, regional stratigraphy and magma evolution / Geological Society, London, Special Publications, 446:173-204, first published on September 30, 2016, doi:10.1144/SP446.2 --- Alexandrina Fulop and Stephan Kurszlaukis: Monogenetic v. polygenetic kimberlite volcanism: in-depth examination of the Tango Extension Super Structure, Attawapiskat kimberlite field, Ontario, Canada / Geological Society, London, Special Publications, 446:205-224, first published on September 23, 2016, doi:10.1144/SP446.7 --- José Jorge Aranda-Gómez, Mariano Cerca, Luis Rocha-Treviño, Jaime Jesús Carrera-Hernández, Gilles Levresse, Jesús Pacheco, Vsevolod Yutsis, Jorge Arturo Arzate-Flores, Elizabeth Chacón, and Hugo Beraldi-Campesi: Structural evidence of enhanced active subsidence at the bottom of a maar: Rincón de Parangueo, México / Geological Society, London, Special Publications, 446:225-254, first published on September 29, 2016, doi:10.1144/SP446.1 --- R. Saucedo, J. L. Macías, Y. Z. E. Ocampo-Díaz, W. Gómez-Villa, E. Rivera-Olguín, R. Castro-Govea, J. M. Sánchez-Núñez, P. W. Layer, J. R. Torres Hernández, and G. Carrasco-Núñez: Mixed magmatic–phreatomagmatic explosions during the formation of the Joya Honda maar, San Luis Potosí, Mexico / Geological Society, London, Special Publications, 446:255-279, first published on February 28, 2017, doi:10.1144/SP446.11 --- Román Alvarez, Fernando Corbo Camargo, Vsevolod V. Yutsis, and Jorge A. Arzate: A volcanic centre in Mexico's Pacific continental shelf / Geological Society, London, Special Publications, 446:281-293, first published on March 3, 2017, doi:10.1144/SP446.12 --- Román Alvarez, Fernando Corbo Camargo, and Vsevolod V. Yutsis: Geophysical modelling of Isla Isabel: a volcanic island on the Mexican continental margin / Geological Society, London, Special Publications, 446:295-310, first published on March 3, 2017, doi:10.1144/SP446.13 --- Walter Báez, Gerardo Carrasco Nuñez, Guido Giordano, José G. Viramonte, and Agostina Chiodi: Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina / Geological Society, London, Special Publications, 446:311-336, first published on September 26, 2016, doi:10.1144/SP446.3 --- Guadalupe Maro and Pablo J. Caffe: Neogene monogenetic volcanism from the Northern Puna region: products and eruptive styles / Geological Society, London, Special Publications, 446:337-359, first published on September 26, 2016, doi:10.1144/SP446.6 --- C. Borrero, H. Murcia, J. Agustin-Flores, M. T. Arboleda, and A. M. Giraldo: Pyroclastic deposits of San Diego maar, central Colombia: an example of a silicic magma-related monogenetic eruption in a hard substrate / Geological Society, London, Special Publications, 446:361-374, first published on December 15, 2016, doi:10.1144/SP446.10
    Pages: Online-Ressource (382 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786202765
    Language: English
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  • 4
    Publication Date: 2019-03-03
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 5
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    In:  http://aquaticcommons.org/id/eprint/14006 | 9596 | 2014-01-21 14:28:19 | 14006 | Gulf and Caribbean Fisheries Institute
    Publication Date: 2021-07-07
    Keywords: Fisheries
    Repository Name: AquaDocs
    Type: conference_item
    Format: application/pdf
    Format: application/pdf
    Format: 1032-1033
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  • 6
    Publication Date: 2021-05-19
    Description: The transports associated with the Subantarctic Front (SAF) and the Polar Front (PF) account for the majority of the volume transport of the Antarctic Circumpolar Current (ACC). After passing through Drake Passage, the SAF and the PF veer northward over the steep topography of the North Scotia Ridge. Interaction of the ACC with the North Scotia Ridge influences the sources of the Malvinas Current. This ridge is a major obstacle to the flow of deep water, with the majority of the deep water passing through the 3100 m deep gap in the ridge known as Shag Rocks Passage. Volume transports associated with these fronts were measured during the North Scotia Ridge Overflow Project, which included the first extensive hydrographic survey of the ridge, carried out in April and May 2003. The total net volume transport northward over the ridge was found to be 117 ± 10 Sv (1 Sv = 106m3s- 1). The total net transport associated with the SAF was approximately 52 ± 4 Sv, and the total transport associated with the PF was approximately 58 ± 5 Sv. Weddell Sea Deep Water was not detected passing through Shag Rocks Passage, contrary to some previous inferences.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: 14-28
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  • 7
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    Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research
    In:  EPIC3Polarforschung, Bremerhaven, Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research, 56(1/2), pp. 43-63, ISSN: 0032-2490
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: "Polarforschung" , peerRev
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  • 8
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    Cambridge University Press
    In:  EPIC3https://www.ipcc.ch/report/ar6/wg2/, Cambridge University Press, pp. 197-377
    Publication Date: 2023-04-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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  • 9
    Publication Date: 2020-02-12
    Description: Harrat Rahat (,10 Ma) is one of the largest volcanic fields on western Arabia. In the north of the field, some of the youngest volcanic centres evolved through either point-like, complex or multiple aligned vents (i.e. along fissures), and have pyroclastic cones, lapilli fall deposits and/ or lava flows associated with them. The products reflect dominantly Hawaiian eruptions, and only one centre experienced phreatomagmatism. Results from new 3He surface-exposure dating provide constraints on stratigraphy of the youngest (,0.3 Ma) products. The rocks are compositionally alkali-basalt and hawaiite, with intra-plate basalt (prevalent mantle (PREMA)) affinity. Each eruption displays a distinct whole-rock composition in an overall linear trend. We suggest that the magma source for each centre is similar, and that composition of the products is different due to different degrees of fractionation. In a single eruption, the magma that reaches the surface first is the least evolved, with the most evolved magma erupting last. We also found that the most primitive magmas erupt less explosively. We think that the degree of magma evolution might correlate with ascent times, assuming that the more evolved magma spent more time en route.We suggest that magma ascent time is likely to be longer than that of other more primitive intra-plate basalts.
    Language: English
    Type: info:eu-repo/semantics/bookPart
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  • 10
    Publication Date: 2020-02-12
    Description: Permafrost landscapes are changing around the Arctic in response to climate warming, with coastal erosion being one of the most prominent and hazardous features. Using drone platforms, satellite images, and historic aerial photographs, we observed the rapid retreat of a permafrost coastline on Qikiqtaruk – Herschel Island, Yukon Territory, in the Canadian Beaufort Sea. This coastline is adjacent to a gravel spit accommodating several culturally significant sites and is the logistical base for the Qikiqtaruk – Herschel Island Territorial Park operations. In this study we sought to (i) assess short-term coastal erosion dynamics over fine temporal resolution, (ii) evaluate short-term shoreline change in the context of long-term observations, and (iii) demonstrate the potential of low-cost lightweight unmanned aerial vehicles (“drones”) to inform coastline studies and management decisions. We resurveyed a 500 m permafrost coastal reach at high temporal frequency (seven surveys over 40 d in 2017). Intra-seasonal shoreline changes were related to meteorological and oceanographic variables to understand controls on intra-seasonal erosion patterns. To put our short-term observations into historical context, we combined our analysis of shoreline positions in 2016 and 2017 with historical observations from 1952, 1970, 2000, and 2011. In just the summer of 2017, we observed coastal retreat of 14.5 m, more than 6 times faster than the long-term average rate of 2.2±0.1 m a−1 (1952–2017). Coastline retreat rates exceeded 1.0±0.1 m d−1 over a single 4 d period. Over 40 d, we estimated removal of ca. 0.96 m3 m−1 d−1. These findings highlight the episodic nature of shoreline change and the important role of storm events, which are poorly understood along permafrost coastlines. We found drone surveys combined with image-based modelling yield fine spatial resolution and accurately geolocated observations that are highly suitable to observe intra-seasonal erosion dynamics in rapidly changing Arctic landscapes.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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