Magma genesis by rifting of oceanic lithosphere above anomalous mantle: Terceira Rift, Azores.

Journal article

Publication Details

Author(s): Beier C, Haase K, Abouchami W, Krienitz MS, Hauff F
Journal: Geochemistry Geophysics Geosystems
Publisher: American Geophysical Union (AGU)
Publication year: 2008
Pages range: doi: 10.1029/2008GC002112
ISSN: 1525-2027
Language: English


The Terceira Rift formed relatively recently (̃1 Ma ago) by rifting of the old oceanic lithosphere of the Azores Plateau and is currently spreading at a rate of 2-4mm/a. Together with the Mid-Atlantic Ridge, the Terceira Rift forms a triple junction that separates the Eurasian, African, and American Plates. Four volcanic systems (São Miguel, João de Castro, Terceira, Graciosa), three of which are islands, are distinguished along the axis and are separated by deep avolcanic basins similar to other ultraslow spreading centers. The major element, trace element and Sr-Nd-Pb isotope geochemistry of submarine and subaerial lavas display large along-axis variations. Major and trace element modeling suggests melting in the garnet stability field at smaller degrees of partial melting at the easternmost volcanic system (São Miguel) compared to the central and western volcanoes, which appear to be characterized by slightly higher melting degrees in the spinel/garnet transition zone. The degrees of partial melting at the Terceira Rift are slightly lower than at other ultraslow mid-ocean ridge spreading axes (Southwest Indian Ridge, Gakkel Ridge) and occur at greater depths as a result of the melting anomaly beneath the Azores. The combined interaction of a high obliquity, very slow spreading rates, and a thick preexisting lithosphere along the axis probably prevents the formation and eruption of larger amounts of melt along the Terceira Rift. However, the presence of ocean islands requires a relatively stable melting anomaly over relatively long periods of time. The trace element and Sr-Nd-Pb isotopes display individual binary mixing arrays for each volcanic system and thus provide additional evidence for focused magmatism with no (or very limited) melt or source interaction between the volcanic systems. The westernmost mantle sources beneath Graciosa and the most radiogenic lavas from the neighboring Mid-Atlantic Ridge suggest a mantle flow from Graciosa toward the Mid-Atlantic Ridge and hence a flux of mantle material from one spreading axis into the other. The Terceira Rift represents a unique oceanic rift system situated within the thickened, relatively old oceanic lithosphere and thus exhibits both oceanic and continental features. © 2008 by the American Geophysical Union.

FAU Authors / FAU Editors

Beier, Christoph PD Dr.
Lehrstuhl für Endogene Geodynamik
Haase, Karsten Prof. Dr.
Lehrstuhl für Endogene Geodynamik

External institutions
Christian-Albrechts-Universität zu Kiel
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
Max-Planck-Institut für Chemie (Otto Hahn Institut) / Max Planck Institute for Chemistry

How to cite

Beier, C., Haase, K., Abouchami, W., Krienitz, M.-S., & Hauff, F. (2008). Magma genesis by rifting of oceanic lithosphere above anomalous mantle: Terceira Rift, Azores. Geochemistry Geophysics Geosystems, doi: 10.1029/2008GC002112.

Beier, Christoph, et al. "Magma genesis by rifting of oceanic lithosphere above anomalous mantle: Terceira Rift, Azores." Geochemistry Geophysics Geosystems (2008): doi: 10.1029/2008GC002112.


Last updated on 2018-16-10 at 19:08