Progressive Changes in Magma Transport at the Active Serreta Ridge, Azores. (28th November 2019)

• Record Type: Journal Article
• Authors: Romer, R.H.W.; Beier, C.; Haase, K.M.; Klügel, A.; Hamelin, C.
• Is Part Of: Geochemistry, geophysics, geosystems. Volume 20:Number 11(2019)
• Page Start: 5394
• Page End: 5414
• Publication Date: 2019-11-28
• Subjects: ocean island -- magmatic -- tectonic -- evolution -- melt transport -- Azores; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 550.5
• DOI: 10.1029/2019GC008562
• Languages: English
• ISSNs: 1525-2027

Abstract

Abstract: Volcanism in the Eastern Azores Plateau occurs at large central volcanoes and along subaerial and submarine fissure zones, resulting from a mantle melting anomaly combined with transtensional stresses. Volcanic structures are aligned WNW‐ESE and NW‐SE, reflecting two tectonic stress fields that control the direction of lateral melt transport. Terceira Island is influenced by both stress fields, dividing the island into an eastern and western part. Several submarine volcanic ridges with variable orientations are located west of Santa Bárbara, the youngest central volcano on Terceira. Major, trace element and Sr‐Nd‐Pb‐Hf isotope compositions from submarine lavas and glasses, in part associated with the 1998–2001 Serreta Ridge eruption, vary between different lava suites, suggesting a formation from different mantle sources. Submarine lavas are more primitive than those from Santa Bárbara volcano, indicating that they are not laterally connected with the shallow magma reservoir located in 2‐ to 5‐km depth beneath the central volcano. Mineral thermobarometric data suggest that the older Serreta magmas were laterally transported at depths >5 km from Santa Bárbara predominantly in WNW direction. We propose that lithospheric extension controls magma transport from the central volcano to Serreta Ridge. The youngest Serreta lavas differ from Santa Bárbara and other submarine ridges in having less radiogenic Pb and higher Hf isotope ratios representing a new magma pulse ascending from the mantle. We conclude that lateral magma transport and the morphology of volcanic ridges are controlled by tectonic stresses in the lithosphere, whereas vertical melt transport is initiated by processes in the mantle. Plain Language Summary: The submarine eruption of lavas along elongated volcanic fissure zones close to volcanic oceanic islands provides the opportunity to chemically decipher the movement of magmas in the crust. Submarine samples from the active Serreta Ridge situated only some 10 km's west of the inhabited island of Terceira in the Azores show that the magmas were transported in the crust at depths of >5 km from the westernmost volcano Santa Bárbara to the site of eruption using pathways predefined by the Azores tectonic situation between the Eurasian and African plates. Lavas from the 1998–2001 eruption of Serreta Ridge, however, indicate that the youngest magmas ascended directly from the mantle through the crust independent of the existing crustal pathways. We interpret the changes in geochemical signals as a transgression from a fissure system being directly related to a central volcano to a new volcanic system acting as a precursor for the formation of a central volcanic edifice west of Santa Bárbara. Key Points: Azores volcanism occurs largely along WNW‐ESE and NW‐SE oriented structures from mantle melting along with transtensional tectonics Serreta Ridge mostly formed by lateral melt transport from a central volcano facilitated by tectonic pathways in the crust The youngest part of Serreta Ridge is the surface expression of a young plumbing system, heralding the formation of a new central volcano