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- W2153424945 abstract "We present seismic investigations of the crustal structure of Tahiti (Society Islands), Rangiroa (Tuamotu Islands), and neighbouring areas. Records from a series of 96 explosions at the short-period stations of the Polynesian Seismic Network form a seismic refraction dataset from which we recover the crustal structures. The crust in the vicinity of Tahiti has the classic structure of 70 Myr-old ocean floor, and features an 8.8 km-thick crust (below sea floor) with 3 7.64–8.25 km s−1 jump at the Mohorovičić (Moho) discontinuity. On the other hand, the Tuamotu plateau shows a very thick crust, reaching 31 km below sea floor, with a 6.83-8.10 km s−1 jump at the Moho. In addition, Rangiroa atoll itself features a 2 km-thick layer of slow material (3.3 km s−1) which we interpret as limestone; comparable structures have been reported at Enewetak and Bikini." @default.
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- W2153424945 date "1987-03-01" @default.
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- W2153424945 title "Crustal structure in the Society and Tuamotu Islands, French Polynesia" @default.
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- W2153424945 doi "https://doi.org/10.1111/j.1365-246x.1987.tb01644.x" @default.
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