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  • 1
    Publication Date: 2016-09-21
    Description: Analysis of abundant plutonic fragments in the voluminous Miocene rhyolitic–basaltic composite ignimbrite P1, the initial felsic cooling unit overlying the basaltic shield on Gran Canaria, helps to solve the problem of bimodal volcanism. Syenogabbros dominate the plutonic suite and provide evidence that magmas of intermediate composition formed abundantly at depth but did not erupt. The entire suite of plutonic fragments comprises (1) pyroxenitic to gabbroic cumulates that directly influenced the liquid line of descent of P1 magmas, (2) gabbro, syenogabbro, syenodiorite and quartz–syenite fragments showing moderate degrees of hydrothermal alteration (chloritization, partial melting), and (3) diverse xenoliths differing significantly in bulk-rock composition and texture from the erupted P1 magmas. The compositions of plutonic series (2) overlap with both bulk-rock and mineral compositions of the erupted magmas, whereas series (1) rocks show lower alkali and silica contents. Compositional variations among the plutonic rocks are compatible with fractional crystallization as the major petrogenetic process, locally modified by magma mixing and selective element contamination. Variations in trace element concentrations of the plutonic rocks, however, are inferred to be the result of evolved interstitial melts penetrating into, or draining out of, crystalline mushes during slow intratelluric solidification. The presence of F-rich amphibole suggests that crystalline mushes were invaded by F-bearing fluids. Overall compositional similarity, and the fact that selective contamination effects are similar, support the interpretation that the series (2) plutonic fragments represent solidified portions of the magmatic system that ultimately produced the erupted P1 magmas. This system extended from the zone of underplating at the mantle–crust boundary through the lower and into the upper crust of Gran Canaria and was roughly vertically zoned in composition as shown by geobarometric calculations.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2021-06-30
    Description: The climactic Los Chocoyos (LCY) eruption from Atitlán caldera (Guatemala) is a key chronostratigraphic marker for the Quaternary period given the extensive distribution of its deposits that reached both the Pacific and Atlantic Oceans. Despite LCY tephra being an important marker horizon, a radioisotopic age for this eruption has remained elusive. Using zircon (U–Th)/He geochronology, we present the first radioisotopically determined eruption age for the LCY of 75 ± 2 ka. Additionally, the youngest zircon crystallization 238U–230Th rim ages in their respective samples constrain eruption age maxima for two other tephra units that erupted from Atitlán caldera, W‐Fall (130 +16/−14 ka) and I‐Fall eruptions (56 +8.2/−7.7 ka), which under‐ and overlie LCY tephra, respectively. Moreover, rim and interior zircon dating and glass chemistry suggest that before eruption silicic magma was stored for 〉80 kyr, with magma accumulation peaking within ca. 35 kyr before the LCY eruption during which the system may have developed into a vertically zoned magma chamber. Based on an updated distribution of LCY pyroclastic deposits, a new conservatively estimated volume of ~1220 ± 150 km3 is obtained (volcanic explosivity index VEI 〉 8), which confirms the LCY eruption as the first‐ever recognized supereruption in Central America.
    Description: Deutsche Forschungsgemeinschaft SCH 2521/6‐1
    Keywords: 551.701 ; 238U–230Th disequilibrium ; geochronology ; tephrochronology ; (U–Th)/He ; zircon
    Type: article
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  • 3
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    In:  UNSPECIFIED, 3 pp.
    Publication Date: 2017-05-22
    Description: (15/05/17 to 21/05/17)
    Type: Report , NonPeerReviewed
    Format: text
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  • 4
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    In:  UNSPECIFIED, 1 pp.
    Publication Date: 2017-05-24
    Description: (22/05/17 to 24/05/17)
    Type: Report , NonPeerReviewed
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  • 5
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    In:  UNSPECIFIED, 2 pp.
    Publication Date: 2018-04-23
    Description: 16/04/18 to 22/04/18
    Type: Report , NonPeerReviewed
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  • 6
    Publication Date: 2017-04-10
    Description: Mildly explosive volcanic eruptions on the deep seafloor have been demonstrated in several cases. In contrast, we present here evidence for highly explosive activity producing diatreme-like ejecta on the surrounding seafloor at the Charles Darwin Volcanic Field (CDVF) located at about 3600 m water depth on the lower southwestern slope of the Cape Verdean Island of Santo Antão. We examined the 1 km diameter Kolá volcanic crater using photogrammetric reconstructions derived from ROV-based imaging followed by 3D quantification using a novel remote sensing workflow. The measured and calculated parameters of physical volcanology derived from the 3D model allow us to get a handle on explosive volcanic processes on the deep seafloor. Kolá crater comprises a complicated lithologic succession of highly fragmented deposits, including spheroidal juvenile lapilli that may contain quenched carbonatite melts, and were likely formed by spray granulation. The deposits comprise numerous well-rounded clasts of MORB-type gabbroic country rocks with diameters up to 20 cm, probably entrained and abraded by fluidization within the vent, that were laterally transported for hundreds of meters through water. In spite of the great depth, the Kolá crater features dense but highly fragmented volcanic deposits with an unexpected combination of large clast sizes and wide clast dispersal. This suggests an energetic eruptive environment which may have similarities with that seen in maar-type eruptions on land. The occurrence of carbonatite in the juvenile clasts provide evidence for a CO2-rich magmatic fluid involved in the explosive events.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
    Publication Date: 2019-09-23
    Description: Sediment gravity cores recovered during the RV METEOR cruise M80/3 in 2010 around the northwestern end of the Cape Verde Archipelago contain three widespread hyaloclastic tephra layers. One of these layers occurs in two sediment cores 40 km apart. The blocky shapes of the vesicle-poor/-free glass-shards clearly indicate their origin from a subaqueous eruption. There are three potential sources in the northwestern Cape Verdean Seamount Province: (1) the Nola Seamount, (2) the Sodade Seamount and (3) the Charles Darwin Volcanic Field. Using geochemical fingerprinting the hyaloclastic glass-shards could be unambiguously correlated to the Charles Darwin Volcanic Field. This is a deep-sea volcanic field consisting of at least 14 eruption centers all at 〉2,850 m below sea level, located about 100 km east of the core locations. Previous studies have documented widespread tephra distributions from relatively shallow (〈 500 mbsl) submarine explosive eruptions, but here we record such a widespread tephra from a deep-sea (probably 〉3000 mbsl) eruption. We discuss the mechanisms of formation and far transport of the hyaloclastic particles.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 8
    Publication Date: 2017-01-17
    Type: Book , NonPeerReviewed
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  • 9
    Publication Date: 2021-03-19
    Description: It is a longstanding observation that the frequency of volcanism periodically changes at times of global climate change. The existence of causal links between volcanism and Earth's climate remains highly controversial, partly because most related studies only cover one glacial cycle. Longer records are available from marine sediment profiles in which the distribution of tephras records frequency changes of explosive arc volcanism with high resolution and time precision. Here we show that tephras of IODP Hole U1437B (northwest Pacific) record a cyclicity of explosive volcanism within the last 1.1 Myr. A spectral analysis of the dataset yields a statistically significant spectral peak at the similar to 100 kyr period, which dominates the global climate cycles since the Middle Pleistocene. A time-domain analysis of the entire eruption and delta O-18 record of benthic foraminifera as climate/sea level proxy shows that volcanism peaks after the glacial maximum and similar to 13 +/- 2 kyr before the delta O-18 minimum right at the glacial/interglacial transition. The correlation is especially good for the last 0.7 Myr. For the period 0.7-1.1 Ma, during the Middle Pleistocene Transition (MPT), the correlation is weaker, since the 100 kyr periodicity in the delta O-18 record diminishes, while the tephra record maintains its strong 100 kyr periodicity.
    Type: Article , PeerReviewed
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  • 10
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    In:  UNSPECIFIED, 2 pp.
    Publication Date: 2018-04-16
    Description: 10/04/18 to 15/04/18
    Type: Report , NonPeerReviewed
    Format: text
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