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  • 1
    Monograph available for loan
    Monograph available for loan
    Methods in sedimentary petrology (1967)
    Stuttgart : Schweizerbart
    Associated volumes
    Details Availability
    Call number: M 93.0401
    In: Sedimentary petrology
    Type of Medium: Monograph available for loan
    Pages: XII, 284 S. : Ill., graph. Darst.
    Series Statement: Sedimentary petrology 1
    Uniform Title: Methoden der Sedimentpetrologie
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Entdecke die Vulkane (2017)
    Münster : Natur und Tier - Verlag GmbH
    Details Availability
    Call number: 22/M 18.91650
    Description / Table of Contents: Vulkane faszinieren uns Menschen schon immer durch ihre spektakulären Ausbrüche. Ungleich bedeutender waren seit jeher die fruchtbaren vulkanischen Böden, gewaltigen Vorräte an Erdwärme und große Schönheit der Vulkane. Die Vulkanexperten Hans-Ulrich Schmincke und Mari Sumita haben in diesem Buch ihr Wissen zusammengefasst, das sie durch Arbeiten auf allen Kontinenten erwarben. Sie erklären auch, mit welchen Methoden Vulkanausbrüche heutzutage erfolgreich vorhergesagt werden können.
    Type of Medium: Monograph available for loan
    Pages: 64 Seiten , farbige Illustrationen , 28 cm, 460 g
    Edition: 2. Auflage
    ISBN: 978-3-86659-384-8
    Series Statement: Entdecke - Die Reihe mit der Eule 32
    URL: Inhaltsverzeichnis
    Language: German
    Branch Library: GFZ Library
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  • 3
    Series available for loan
    Series available for loan
    Phreatomagmatische Phasen in quartären Vulkanen der Osteifel (1977)
    Hannover : Schweizerbart
    Associated volumes
    Details Availability
    Call number: SR 90.0066(39)
    In: Geologisches Jahrbuch
    Type of Medium: Series available for loan
    Pages: 48 S.
    Series Statement: Geologisches Jahrbuch : Reihe A 39
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Pyroclastic rocks (1984)
    Berlin [u.a.] : Springer
    Details Availability
    Call number: M 92.0939 ; M 92.1193 ; AWI G1-92-0382
    Type of Medium: Monograph available for loan
    Pages: XIV, 472 S.
    ISBN: 3540513418
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Vulkanismus (1986)
    Darmstadt : Wissenschftl. Buchges.
    Details Availability
    Call number: M 92.0848
    Type of Medium: Monograph available for loan
    Pages: VII, 164 S. : Ill. (z.T. farb.)
    ISBN: 3534076222
    Classification:
    A.3.1.
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 6
    Monograph available for loan
    Monograph available for loan
    Vulkanismus (2000)
    Darmstadt : Wiss. Buchges.
    Details Availability
    Call number: 9/M 01.0091 ; PIK N 411-00-0024
    Type of Medium: Monograph available for loan
    Pages: 264 S. : zahlr. Farbabb.
    Edition: 2., überarb. und erw. Aufl.
    ISBN: 3534141024
    Classification:
    Petrology, Petrography
    Location: Reading room
    Location: A 18 - must be ordered
    Branch Library: GFZ Library
    Branch Library: PIK Library
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  • 7
    Monograph available for loan
    Monograph available for loan
    Volcanism (2004)
    Berlin [u.a.] : Springer
    Details Availability
    Call number: 9/M 04.0546
    Description / Table of Contents: Volcanic eruptions are the clear and dramatic expression of dynamic processes in planet Earth. The author explains in a concise and easy to understand manner the basics and most recent findings in the field. Based on over 300 color figures and the model of plate tectonics, the book offers insight into the generation of magmas and the occurrence and origin of volcanoes. The analysis and description of volcanic structures is followed by process oriented chapters discussing the role of magmatic gases as well as explosive mechanisms and sedimentation of volcanic material. The final chapters deal with the forecast of eruptions and their influence on climate.
    Type of Medium: Monograph available for loan
    Pages: X, 324 S. , Ill., graph. Darst., Kt.
    ISBN: 3540436502
    Classification:
    Petrology, Petrography
    Location: Reading room
    Branch Library: GFZ Library
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  • 8
    Monograph available for loan
    Monograph available for loan
    Vulkanismus (2013)
    Darmstadt : WBG (Wiss. Buchges.)
    Details Availability
    Call number: 9/M 17.90844 ; 9/M 17.90844(2. Ex.)
    Type of Medium: Monograph available for loan
    Pages: 264 S. , zahlr. Ill., graph. Darst., Kt.
    Edition: 4., unveränd. Aufl.
    ISBN: 9783534262458
    URL: Inhaltsverzeichnis
    Parallel Title: Erscheint auch als Vulkanismus
    Language: German
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 9
    Electronic Resource
    Electronic Resource
    Rates of magma ascent and depths of magma reservoirs beneath La Palma (Canary Islands) (1997)
    Oxford, UK : Blackwell Science Ltd
    Terra nova 9 (1997), S. 0 
    Details
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Peridotitic mantle xenoliths from historic and prehistoric eruptions on La Palma show many similarities. Prolonged reactions of the xenoliths with their host magmas have been used to place constraints on the magma transport system beneath the island. All xenoliths show crystalline selvages and 0.9–2.6 mm wide diffusion zones in olivine along most of their surface. Diffusion kinetics in olivine, combined with fluid inclusion barometry, document that selvages and diffusion zones formed at crustal levels within 8 to about 100 years. Some xenolith fractures lack selvages and were in contact with the host magma for less than 4 days. A multistage magma ascent is proposed: (i) peridotite wall rock was fragmented and became incorporated into the ascending magma years to decades prior to the eruption; (ii) the xenoliths were rapidly transported to, and deposited in, crustal magma reservoirs, forming selvages and diffusion zones at the xenolith rims; (iii) renewed fragmentation of the xenoliths occurred days to hours prior to eruption, possibly by decompressive strain fracturing during rapid ascent.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3121.1997.d01-15.x
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  • 10
    Electronic Resource
    Electronic Resource
    Reflection Seismic Investigations In the Volcaniclastic Apron of Gran Canaria and Implications For Its Volcanic Evolution (1996)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 125 (1996), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: High-resolution reflection seismic data obtained around Gran Canaria allow a detailed and consistent correlation of seismic reflectors of the northern and southern Canary Basins with the lithology drilled by DSDP Leg 47A SSE of Gran Canaria, as well as with major phases of volcanic activity on Gran Canaria as mapped onshore. Two prominent reflectors were chosen as marker horizons and correlated with the drilled lithology. the results indicate that reflector R7 above the Miocene volcaniclastic debris flows V1-V3 reflects the shield-building phase of Gran Canaria. Reflector R3 is interpreted as corresponding with the Pliocene Roque Nublo formation.The top of the massive island flank of Gran Canaria, defined by seismically chaotic facies, extends 44 to 72 km off the coast of Gran Canaria. West of Gran Canaria the flank of Tenerife onlaps the steeper and older flank of Gran Canaria, which, in turn, is onlapping the older flank of Fuerteventura to the east in a similar way.Erosional channels, which can also be traced up to 50 km from the area between Gran Canaria and Fuerteventura into the deeper northern basin, have been identified in the bathymetry.The data presented provide new detailed information for modelling the submarine and subaerial evolution of the central Canary Islands of Gran Canaria and Tenerife, i.e. the timing of their shield-building phases and later stages of major volcanic activity, as reflected by the position of prominent seismic reflectors in the seismic stratigraphy.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1996.tb00015.x
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