SHRIMP Pb/U zircon ages constrain gabbroic crustal accretion at Atlantis Bank on the ultraslow-spreading Southwest Indian Ridge
Absolute ages of plutonic rocks from mid-ocean ridges provide important constraints on the scale, timing and rates of oceanic crustal accretion, yet few such rocks have been absolutely dated. We present 206Pb/ 238U SHRIMP zircon ages from two ODP Drill Holes and a surface sample from Atlantis Bank o...
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Veröffentlicht in: | Earth and planetary science letters 2009-10, Vol.287 (3), p.540-550 |
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