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Magmatism in Subduction Zones
đ Subduction zones exhibit magmatic rocks such as andesites, rhyolites (microcrystalline texture, rapid cooling), and plutonic/acidic rocks (fully crystallized, slow cooling).
đ These rocks indicate the presence of magma formation originating from partial melting of peridotite in the mantle.
â The central question addressed is how magma forms within subduction zones.
Geothermal Gradient vs. Peridotite Melting
đĄïž The red curve shows the geothermal gradient in subduction zones: temperature is slightly below at depth and slightly below at depth.
đ§Ș Laboratory experiments on dry peridotite define the dry solidus (limit between solid and partially liquid) and the liquidus (limit between partially liquid and fully liquid).
â Theoretically, the subduction zone geothermal gradient never crosses the dry peridotite solidus, meaning dry peridotite should never partially melt under these conditions.
The Role of Hydration in Melting
đ§ Experiments using hydrated peridotite (e.g., serpentinites) show a significantly lower partial melting temperature compared to dry peridotite.
đ„ At depth, the partial melting temperature for hydrated peridotite is about , whereas for dry peridotite it is around .
â
The geothermal gradient in subduction zones intersects the hydrated peridotite solidus between approximately and depth, creating a window for partial melting.
Key Points & Insights
âĄïž Magmatic rocks in subduction zones are definitively sourced from partial melting of peridotite in the mantle.
âĄïž The reason melting occurs is that the subducting slab carries water (hydration) into the mantle, which lowers the solidus temperature of the surrounding peridotite.
âĄïž Melting is confined to a specific depth range ( to ), indicating that hydrated peridotite must exist below the subduction zone where temperatures are sufficient.
đž Video summarized with SummaryTube.com on Jan 06, 2026, 19:05 UTC
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Full video URL: youtube.com/watch?v=l7Jjspw-TFM
Duration: 6:28
Get instant insights and key takeaways from this YouTube video by Mon Cours De SVT.
Magmatism in Subduction Zones
đ Subduction zones exhibit magmatic rocks such as andesites, rhyolites (microcrystalline texture, rapid cooling), and plutonic/acidic rocks (fully crystallized, slow cooling).
đ These rocks indicate the presence of magma formation originating from partial melting of peridotite in the mantle.
â The central question addressed is how magma forms within subduction zones.
Geothermal Gradient vs. Peridotite Melting
đĄïž The red curve shows the geothermal gradient in subduction zones: temperature is slightly below at depth and slightly below at depth.
đ§Ș Laboratory experiments on dry peridotite define the dry solidus (limit between solid and partially liquid) and the liquidus (limit between partially liquid and fully liquid).
â Theoretically, the subduction zone geothermal gradient never crosses the dry peridotite solidus, meaning dry peridotite should never partially melt under these conditions.
The Role of Hydration in Melting
đ§ Experiments using hydrated peridotite (e.g., serpentinites) show a significantly lower partial melting temperature compared to dry peridotite.
đ„ At depth, the partial melting temperature for hydrated peridotite is about , whereas for dry peridotite it is around .
â
The geothermal gradient in subduction zones intersects the hydrated peridotite solidus between approximately and depth, creating a window for partial melting.
Key Points & Insights
âĄïž Magmatic rocks in subduction zones are definitively sourced from partial melting of peridotite in the mantle.
âĄïž The reason melting occurs is that the subducting slab carries water (hydration) into the mantle, which lowers the solidus temperature of the surrounding peridotite.
âĄïž Melting is confined to a specific depth range ( to ), indicating that hydrated peridotite must exist below the subduction zone where temperatures are sufficient.
đž Video summarized with SummaryTube.com on Jan 06, 2026, 19:05 UTC
Find relevant products on Amazon related to this video
Science
Shop on Amazon
Laboratory
Shop on Amazon
Experiment
Shop on Amazon
Neuroscience Book
Shop on Amazon
As an Amazon Associate, we earn from qualifying purchases

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