2022
DOI: 10.1029/2022gl100395
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Gas Migration Episodes Observed During Peridotite Alteration in the Samail Ophiolite, Oman

Abstract: The peridotites constituting the Earth's upper mantle are highly reactive when exposed to aqueous fluids under near-surface conditions (Kelemen & Hirth, 2012). Peridotite alteration is a major transfer process for volatiles between the hydrosphere and the lithosphere (Guillot & Hattori, 2013), and in the presence of carbon-bearing fluids it leads to carbonate precipitation (Power et al., 2013), which represents a natural mechanism for carbon capture and storage (Kelemen & Matter, 2008). Peridotite alteration i… Show more

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Cited by 3 publications
(4 citation statements)
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“…However this is not the case (ρ = −0.0225). These fracture networks must act as fluid pathways given adequate fluid pressures, and this fluid motion is detected acoustically in BA1B (Aiken et al, 2022).…”
Section: Discussionmentioning
confidence: 99%
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“…However this is not the case (ρ = −0.0225). These fracture networks must act as fluid pathways given adequate fluid pressures, and this fluid motion is detected acoustically in BA1B (Aiken et al, 2022).…”
Section: Discussionmentioning
confidence: 99%
“…The decrease in the extent of peridotite alteration with depth may suggest that significant peridotite alteration in the region has been relatively young, within the last 50,000 years . H 2 and CH 4 outgassing have previously been detected in the Oman boreholes and are possible products of ongoing peridotite alteration Aiken et al, 2022).…”
Section: Introductionmentioning
confidence: 87%
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“…However, in many porous systems, several fluid phases, including water, gas, and different immiscible fluids, coexist in the pore space (Blunt, 2017; Holtzman et al., 2020; Zhao et al., 2016). Dispersion in such multiphase flows affects several important processes, including contaminant and nutrient transport in soils and catchments (e.g., Kirchner et al., 2000; Sebilo et al., 2013), brine and nutrient transport in snow and sea ice (e.g., Golden, 2001; Waldner et al., 2004), CO 2 sequestration in geological reservoirs (e.g., Szulczewski et al., 2012; Zheng et al., 2017), underground hydrogen storage (Lysyy et al., 2022; Tarkowski, 2019), and solute dispersion in gas seepage sites (e.g., Aiken et al., 2022; Scandella et al., 2016).…”
Section: Introductionmentioning
confidence: 99%