The lithospheric shear-wave velocity structure of Saudi Arabia: Young volcanism in an old shield
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文摘

We find high Vp/Vs ratios at Harrat Lunayyir, likely resulting from old dyke intrusions.

We find low Vs and high temperature of mantle-lid at the southern/northern Arabian shield.

The Vs and temperature patterns are due to thermal conduction from the Afar/Jordan plume.

The volcanism of western Arabia may be due to small-scale adiabatic ascent of magma diapirs.

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