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18 Terms
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Anhydrous melting
melting temperature increases with increasing pressure - under dry conditions
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Silicate melt is less \____ than solid rock
dense
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As melting progresses
liquid will segregate from the solid residuum and ascend to the earth's surface
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Melting mechanisms process
1. mantle rises towards the surface from point a will intersect with solidus on point b 2. at point b, the rising mantle will begin to melt 3. therefore melting ensues when mantle material moves to lower pressure or shallower depth
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decompression melting
melting that occurs as rock ascends due to a drop in confining pressure - occurs in passve respones to lithosphereic stretching and thinning as plates are pulled apart - occurs in actively upwelling, convecting mantle
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Decompression melting occurs at
divergent margins and beneath plate interiors
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oceanic lithosphere is created at
divergent margins
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Plume
known as hot spots - active decompression melting
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The heat associated with plumes creates
elevated topography
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Large volumes of magma are erupted from
the heads of plumes - preserved in flood basalt provinces on continents
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Oceanic plateaus form from
immense short-lived eruptions of basalt
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Most recent volcanoes are located at
constructive and destructive plate margins
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Melting to produce magmas must occur
in the mantle beneath lies of active volcanism
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volcanism at convergent margins
- often explosive - eruptions release large quantities of water
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Water dramatically lowers
the melting temperature of pure minerals - relative to the melting temperature under anhydrous conditions - melting temperature decreases ith increasing pressure
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Addition of water to the mantle may trigger
melting at subduction zones
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Interaction of seawater and basalt
seawater oceanic crust penetrates along fractures - water is heated and reacts with basalt to form hydrated oceanic crust
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Magma genesis
1. Melting occurs beneath a mid-ocean ridge 2. mantle plume and a hot-spot volcano 3. subduction yields a volcanic arc