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1000 Titel
  • Timescales from magma mixing to eruption in alkaline volcanism in the Eifel volcanic fields, western Germany
1000 Autor/in
  1. Sundermeyer, Caren |
  2. Gätjen, Jochen |
  3. Weimann, Lena |
  4. Wörner, Gerhard |
1000 Erscheinungsjahr 2020
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2020-07-25
1000 Erschienen in
1000 Quellenangabe
  • 175(8):77
1000 Copyrightjahr
  • 2020
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00410-020-01715-y |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>Diffusion profiles in olivine crystals from the final mafic eruption products of the compositionally zoned Laacher See tephra deposit were measured to identify recharge and eruption-triggering events prior to the eruption of the Laacher See volcano (12.9 kyr). These products represent the hybrids of mixing between phonolite and intruding basanite at the bottom of the reservoir, which is likely related to the eruption-triggering event. Additionally, olivine crystals from ten basanitic scoria cones and maar deposits (East Eifel) and two nephelinites (West Eifel) were analyzed to constrain histories of olivine in Quaternary basanite magmas. Olivine crystals from the Laacher See hybrids vary in core composition (Fo<jats:sub>83–89</jats:sub>) and show reversely zoned mantles with high Fo<jats:sub>87.8–89</jats:sub> compared to olivine in East Eifel basanites erupted in nearby, older scoria cones. Towards the crystal margin, olivine in the hybrids develop a normally zoned overgrowth (Fo<jats:sub>86.5–87.5</jats:sub>). Olivine from East Eifel basanites show similar zonation and core compositions (Fo<jats:sub>80–88</jats:sub>) but have less forsteritic mantles (Fo<jats:sub>83–88</jats:sub>) indicating that these basanites are less primitive than those recharging the Laacher See reservoir (&gt; Fo<jats:sub>89</jats:sub>). Olivine in the West Eifel nephelinites show mantles similar to those from Laacher See (Fo<jats:sub>87.5–90</jats:sub>), but have normal zoning and high-Fo cores (Fo<jats:sub>88–92</jats:sub>). This indicates that olivine in the Laacher See hybrids were entrained by a near-primary basanite from older cumulates just before hybridization of the basanite with the phonolite. Diffusion modeling indicates maximum timescales between entrainment and eruption of Laacher See of 30–400 days that are comparable to those calculated for olivine from basanitic scoria cones (10–400 days).</jats:p>
1000 Sacherschließung
lokal Diffusion
lokal Olivine
lokal Original Paper
lokal Mixing
lokal Timescales
lokal Zoning
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0003-4330-4656|https://frl.publisso.de/adhoc/uri/R8OkdGplbiwgSm9jaGVu|https://frl.publisso.de/adhoc/uri/V2VpbWFubiwgTGVuYQ==|https://frl.publisso.de/adhoc/uri/V8O2cm5lciwgR2VyaGFyZA==
1000 Hinweis
  • DeepGreen-ID: 89717026295645fa82694c2632a7a3c6 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
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1000 Erstellt am 2023-11-18T00:00:44.439+0100
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1000 Zuletzt bearbeitet 2023-12-01T10:08:33.253+0100
1000 Objekt bearb. Fri Dec 01 10:08:33 CET 2023
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