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Sigmundsson F, Parks M, Geirsson H, Hooper A, Drouin V, Vogfjörd KS, Ófeigsson BG, Greiner SHM, Yang Y, Lanzi C, De Pascale GP, Jónsdóttir K, Hreinsdóttir S, Tolpekin V, Friðriksdóttir HM, Einarsson P, Barsotti S. Fracturing and tectonic stress drive ultrarapid magma flow into dikes. Science 2024; 383:1228-1235. [PMID: 38330140 DOI: 10.1126/science.adn2838] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/02/2023] [Accepted: 01/29/2024] [Indexed: 02/10/2024]
Abstract
Many examples of exposed giant dike swarms can be found where lateral magma flow has exceeded hundreds of kilometers. We show that massive magma flow into dikes can be established with only modest overpressure in a magma body if a large enough pathway opens at its boundary and gradual buildup of high tensile stress has occurred along the dike pathway prior to the onset of diking. This explains rapid initial magma flow rates, modeled up to about 7400 cubic meters per second into a dike ~15-kilometers long, which propagated under the town of Grindavík, Southwest Iceland, in November 2023. Such high flow rates provide insight into the formation of major dikes and imply a serious hazard potential for high-flow rate intrusions that propagate to the surface and transition into eruptions.
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Affiliation(s)
- Freysteinn Sigmundsson
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | - Michelle Parks
- Icelandic Meteorological Office, IS-105 Reykjavik, Iceland
| | - Halldór Geirsson
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | - Andrew Hooper
- COMET, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK
| | - Vincent Drouin
- Icelandic Meteorological Office, IS-105 Reykjavik, Iceland
| | | | | | - Sonja H M Greiner
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
- Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden
- Center for Natural Hazard and Disaster Science, 752 36 Uppsala/Stockholm/Karlstad, Sweden
| | - Yilin Yang
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | - Chiara Lanzi
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | - Gregory P De Pascale
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | | | | | | | | | - Páll Einarsson
- Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland
| | - Sara Barsotti
- Icelandic Meteorological Office, IS-105 Reykjavik, Iceland
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El Bilali H, Ernst RE. Far-travelled 3700 km lateral magma propagation just below the surface of Venus. Nat Commun 2024; 15:1759. [PMID: 38409271 PMCID: PMC10897134 DOI: 10.1038/s41467-024-45603-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/13/2023] [Accepted: 01/30/2024] [Indexed: 02/28/2024] Open
Abstract
The Great Dyke of Atla Regio (GDAR) is traced for ~3700 km on Venus, as a surface graben (narrow trough) interpreted to overlie a continuous laterally-emplaced underlying mafic dyke (vertical magma-filled crack). The GDAR belongs to a giant radiating dyke swarm associated with Ozza Mons (volcano), Atla Regio plume, and was fed from a magma reservoir ~600 km south of the Ozza Mons centre. A 50-degree counter-clockwise swing of the GDAR at 1200 km from the centre is consistent with a 1200 km radius for the underlying Ozza Mons plume head, and a stress link to the 10,000 km long Parga Chasmata rift system. Our discovery of the GDAR, should spur the search for additional long continuous single dykes on Venus (and Earth), with implications for estimating plume head size, locating buffered magma reservoirs, mapping regional stress variation at a geological instant, and revealing relative ages (through cross-cutting relationships) over regional-scale distances.
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Affiliation(s)
- H El Bilali
- Department of Earth Sciences, Carleton University, Ottawa, ON, Canada.
| | - R E Ernst
- Department of Earth Sciences, Carleton University, Ottawa, ON, Canada.
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Bland MT, Elder CM. Silicate Volcanism on Europa's Seafloor and Implications for Habitability. GEOPHYSICAL RESEARCH LETTERS 2022; 49:e2021GL096939. [PMID: 35866068 PMCID: PMC9286870 DOI: 10.1029/2021gl096939] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 11/08/2021] [Revised: 01/27/2022] [Accepted: 01/28/2022] [Indexed: 06/15/2023]
Abstract
Habitable ocean environments on Europa require an influx of reactants to maintain chemical disequilibrium. One possible source of reactants is seafloor volcanism. Modeling has shown that dissipation of tidal energy in Europa's asthenosphere can generate melt, but melt formation cannot be equated with volcanism. Melt must also be transported through Europa's cold lithosphere to erupt at the seafloor. Here, we use two models of dike propagation to show that dikes can only traverse the lithosphere if either the fracture toughness of the lithosphere or the flux into the dike is large (>500 MPa m1/2 or ∼1 m2 s-1, respectively). We conclude that cyclic volcanic episodes might provide reactants to Europa's ocean if magma accumulates at the base of the lithosphere for several thousand years. However, if dikes form too frequently, or are too numerous, the magma flux into each will be insufficient, and volcanism cannot support a habitable ocean environment.
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Affiliation(s)
- M. T. Bland
- Astrogeology Science CenterU. S. Geological SurveyFlagstaffAZUSA
| | - C. M. Elder
- Jet Propulsion LaboratoryCalifornia Institute of TechnologyPasadenaCAUSA
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Temporal Evolution of Cooling by Natural Convection in an Enclosed Magma Chamber. Processes (Basel) 2022. [DOI: 10.3390/pr10010108] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/17/2022] Open
Abstract
This research numerically studies the transient cooling of partially liquid magma by natural convection in an enclosed magma chamber. The mathematical model is based on the conservation laws for momentum, energy and mass for a non-Newtonian and incompressible fluid that may be modeled by the power law and the Oberbeck–Boussinesq equations (for basaltic magma) and solved with the finite volume method (FVM). The results of the programmed algorithm are compared with those in the literature for a non-Newtonian fluid with high apparent viscosity (10–200 Pa s) and Prandtl (Pr = 4 × 104) and Rayleigh (Ra = 1 × 106) numbers yielding a low relative error of 0.11. The times for cooling the center of the chamber from 1498 to 1448 K are 40 ky (kilo years), 37 and 28 ky for rectangular, hybrid and quasi-elliptical shapes, respectively. Results show that for the cases studied, natural convection moved the magma but had no influence on the isotherms; therefore the main mechanism of cooling is conduction. When a basaltic magma intrudes a chamber with rhyolitic magma in our model, natural convection is not sufficient to effectively mix the two magmas to produce an intermediate SiO2 composition.
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Le Mével H, Gregg PM, Feigl KL. Magma injection into a long-lived reservoir to explain geodetically measured uplift: Application to the 2007-2014 unrest episode at Laguna del Maule volcanic field, Chile. JOURNAL OF GEOPHYSICAL RESEARCH. SOLID EARTH 2016; 121:6092-6108. [PMID: 27867790 PMCID: PMC5101856 DOI: 10.1002/2016jb013066] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/06/2016] [Revised: 07/06/2016] [Accepted: 07/09/2016] [Indexed: 06/02/2023]
Abstract
Moving beyond the widely used kinematic models for the deformation sources, we present a new dynamic model to describe the process of injecting magma into an existing magma reservoir. To validate this model, we derive an analytical solution and compare its results to those calculated using the Finite Element Method. A Newtonian fluid characterized by its viscosity, density, and overpressure (relative to the lithostatic value) flows through a vertical conduit, intruding into a reservoir embedded in an elastic domain, leading to an increase in reservoir pressure and time-dependent surface deformation. We apply our injection model to Interferometric Synthetic Aperture Radar (InSAR) data from the ongoing unrest episode at Laguna del Maule (Chile) volcanic field that started in 2007. Using a grid search optimization, we minimize the misfit to the InSAR displacement data and vary the three parameters governing the analytical solution: the characteristic timescale τP for magma propagation, the maximum injection pressure, and the inflection time when the acceleration switches from positive to negative. For a spheroid with semimajor axis a = 6200 m, semiminor axis c = 100 m, located at a depth of 4.5 km in a purely elastic half-space, the best fit to the InSAR displacement data occurs for τP =9.5 years and an injection pressure rising up to 11.5 MPa for 2 years. The volume flow rate increased to 1.2 m3/s for 2 years and then decreased to 0.7 m3/s in 2014. In 7.3 years, at least 187 × 106 m3 of magma was injected.
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Affiliation(s)
- Hélène Le Mével
- Department of GeoscienceUniversity of Wisconsin–MadisonMadisonWisconsinUSA
| | - Patricia M. Gregg
- Department of GeologyUniversity of Illinois at Urbana–ChampaignChampaignIllinoisUSA
| | - Kurt L. Feigl
- Department of GeoscienceUniversity of Wisconsin–MadisonMadisonWisconsinUSA
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Ishizuka O, Geshi N, Itoh J, Kawanabe Y, TuZino T. The magmatic plumbing of the submarine Hachijo NW volcanic chain, Hachijojima, Japan: Long-distance magma transport? ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2007jb005325] [Citation(s) in RCA: 28] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Osamu Ishizuka
- Institute of Geology and Geoinformation; Geological Survey of Japan/AIST; Tsukuba Japan
| | - Nobuo Geshi
- Institute of Geology and Geoinformation; Geological Survey of Japan/AIST; Tsukuba Japan
| | - Jun'ichi Itoh
- Institute of Geology and Geoinformation; Geological Survey of Japan/AIST; Tsukuba Japan
| | - Yoshihisa Kawanabe
- Institute of Geology and Geoinformation; Geological Survey of Japan/AIST; Tsukuba Japan
| | - Taqumi TuZino
- Institute of Geology and Geoinformation; Geological Survey of Japan/AIST; Tsukuba Japan
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Connolly JAD, Podladchikov YY. Decompaction weakening and channeling instability in ductile porous media: Implications for asthenospheric melt segregation. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2005jb004213] [Citation(s) in RCA: 95] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Buck WR, Einarsson P, Brandsdóttir B. Tectonic stress and magma chamber size as controls on dike propagation: Constraints from the 1975-1984 Krafla rifting episode. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2005jb003879] [Citation(s) in RCA: 168] [Impact Index Per Article: 9.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- W. Roger Buck
- Lamont-Doherty Earth Observatory; Columbia University; Palisades New York USA
| | - Páll Einarsson
- Institute of Earth Sciences; University of Iceland; Reykjavík Iceland
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