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- W2092713527 abstract "For the first time, the crystallized remnant of an oceanic ridge magma chamber is documented in the Oman ophiolite. It exists in the centre of a 40 km long monoclinal ridge (Jebel Dihm, Wadi Tayin massif), exposing a full crustal section perpendicular to the spreading direction. New detailed mapping supported by U-Pb zircon geochronology suggests that the active, fast-spreading ridge that died just prior to detachment of the ophiolite is preserved and largely intact. Our observations provide insights into the crystallizing mush zone of a magma chamber, before it crosses the external walls and solidifies as deformed gabbros. Our data provide new constraints on the shape and internal dynamics of a magma chamber, including gabbro subsidence from the floor of a perched melt lens and the limited contribution of sills to crustal accretion. By locating precisely the palaeo-ridge axis, prior full spreading rate estimates can be increased to ~140 km Ma−1." @default.
- W2092713527 created "2016-06-24" @default.
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- W2092713527 date "2015-01-22" @default.
- W2092713527 modified "2023-10-14" @default.
- W2092713527 title "Inside the magma chamber of a dying ridge segment in the Oman ophiolite" @default.
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- W2092713527 doi "https://doi.org/10.1111/ter.12130" @default.
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