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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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East Pacific Ocean Islands
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Easter Island (1)
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Oceania
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Polynesia
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Cook Islands (1)
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French Polynesia
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Austral Islands (1)
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Marquesas Islands (1)
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Pacific Ocean
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East Pacific
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Southeast Pacific (1)
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South Pacific
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Louisville Ridge (1)
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Southeast Pacific (1)
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United States
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Michigan (1)
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elements, isotopes
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isotope ratios (1)
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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stable isotopes
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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metals
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lead
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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geochronology methods
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K/Ar (1)
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geologic age
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts (1)
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Primary terms
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absolute age (1)
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene (1)
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East Pacific Ocean Islands
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Easter Island (1)
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geochemistry (1)
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geophysical methods (1)
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igneous rocks
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volcanic rocks
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basalts (1)
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-
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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stable isotopes
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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-
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lava (1)
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mantle (2)
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metals
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lead
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Pb-206/Pb-204 (1)
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Pb-208/Pb-204 (1)
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-
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ocean floors (1)
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Oceania
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Polynesia
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Cook Islands (1)
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French Polynesia
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Austral Islands (1)
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Marquesas Islands (1)
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-
-
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Pacific Ocean
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East Pacific
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Southeast Pacific (1)
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South Pacific
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Louisville Ridge (1)
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Southeast Pacific (1)
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-
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plate tectonics (2)
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reefs (1)
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sedimentary rocks
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carbonate rocks (1)
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United States
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Michigan (1)
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well-logging (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks (1)
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Time-lapse borehole gravity imaging of CO 2 injection and withdrawal in a closed carbonate reef
Introduction to special section: CO 2 storage and utilization
Hotspot theory was first proposed on the basis of the observation of linear volcanic chains on the Pacific plate and assumed age progression within these chains. Knowledge of the ages of islands and seamounts is therefore of primary importance to analyzing intraplate volcanism and deciphering the history of hotspot tracks. In this paper we review published radiometric ages of islands and seamounts on the Pacific plate to help further reconstruction. We present a compilation of 1645 radiometric ages sorted by chain and further by island or seamount, along with a brief overview of each chain. Paleomagnetic ages obtained from seamount magnetism have not been considered, except for some oceanic plateaus (e.g., Shatsky rise). We do not consider foraminifer ages, which only give minimum ages of seamounts. Reliability problems intrinsic to the samples and to the radiometric dating methods must be considered. Dating of whole rocks must generally be disregarded unless they have been subject to special treatment, Ar/Ar incremental heating dating should be preferred over other methods, and data that do not pass the reliability criteria discussed by Baksi (this volume) should be disregarded. Thus use of the ages compiled in our database must be done in the light of filtering, and we encourage the user to check critically the initial papers in which the dates were published.