Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/89854
Title: How magmatic storage regions attract and repel propagating dikes
Authors: Pansino, Stephen
Taisne, Benoit
Keywords: Magma Storage Region
Dike Propagation
Science::Geology
Issue Date: 2018
Source: Pansino, S., & Taisne, B. (2019). How magmatic storage regions attract and repel propagating dikes. Journal of Geophysical Research: Solid Earth, 124(1), 274-290. doi:10.1029/2018JB016311
Series/Report no.: Journal of Geophysical Research: Solid Earth
Abstract: We investigate the effect of magmatic reservoir pressure on the propagation of dikes that approach from below, using analogue experiments. We injected oil into gelatin and observed how dike propagation responded to the stress field around a pressurized, spherical reservoir, filled with water. The reservoir was modeled using two different setups: one simply using an inflatable rubber balloon and the other by constructing a liquid‐filled cavity. We find that the dike's response is dependent on the sign of the reservoir pressure (i.e., inflated/overpressurized and deflated/underpressurized) as well as on the dike's initial orientation (i.e., if its strike is radially, circumferentially, or obliquely oriented to the reservoir). Dikes that are initially strike radial respond, respectively, by propagating toward or away from overpressurized or underpressurized reservoirs, taking advantage of the reservoir's hoop stresses. Otherwise‐oriented dikes respond by changing orientation, twisting and curling into a form dictated by the principal stresses in the medium. For overpressurized reservoirs, they are coaxed to propagate radially to, and therefore approach, the reservoir. For underpressurized reservoirs, they generally reorient to propagate tangentially, which causes them to avoid the reservoir. The magnitude of reservoir pressure controls at which distance dikes can be affected, and, at natural scales, we estimate that this occurs within a radius of a few tens of kilometers. This diminishes with time, due to viscous stress relaxation of the crust, which will occur on a timescale of hundreds of years.
URI: https://hdl.handle.net/10356/89854
http://hdl.handle.net/10220/49333
ISSN: 2169-9356
DOI: 10.1029/2018JB016311
Rights: © 2018 The Author(s). This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:ASE Journal Articles
EOS Journal Articles

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