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Paul R. Renne

Researcher at Berkeley Geochronology Center

Publications -  374
Citations -  32299

Paul R. Renne is an academic researcher from Berkeley Geochronology Center. The author has contributed to research in topics: Basalt & Lava. The author has an hindex of 89, co-authored 363 publications receiving 29354 citations. Previous affiliations of Paul R. Renne include University of California, Berkeley & Planetary Science Institute.

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Eruptive history and petrologic evolution of the Albano multiple maar (Alban Hills, Central Italy)

TL;DR: A comprehensive study of the Albano multiple maar (Alban Hills, Italy) using 40Ar/39Ar geochronology of the most complete stratigraphic section and other proximal and distal outcrops is presented in this paper.
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Intercalibration and age of the Alder Creek sanidine 40Ar/39Ar standard

TL;DR: In this paper, the Alder Creek sanidine (ACs) was calculated using three mass spectrometers and various irradiation and analytical protocols, yielding a weighted mean R F C s A C s ǫ = 0.041702 −0.000014 (σ).
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40Ar/39Ar dating of 1.0–1.1 Ga magnetizations from the Sa˜o Francisco and Kalahari cratons: tectonic implications for Pan-African and Brasiliano mobile belts

TL;DR: In this article, the ages of dykes from 1.1-1.0 Ga dyke swarms in eastern Brazil (Sa˜o Francisco Craton) are compared with granulites of the Namaqua Province in southern Africa (Kalahari Graton), indicating that the intervening Pan African (Brasiliano) mobile belt may record a craton-craton collision.
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U/Pb and Pb/Pb zircon ages for arc-related intrusions of the Bolu Massif (W Pontides, NW Turkey): evidence for Late Precambrian (Cadomian) age

TL;DR: In this article, the authors presented new U/Pb and Pb/pb radiometric age data from two tectono-stratigraphic units of the regionally extensive Bolu Massif, in the W Pontides Fragment, N Turkey.
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The 40Ar/39Ar and K/Ar dating of lavas from the Hilo 1‐km core hole, Hawaii Scientific Drilling Project

TL;DR: In this article, the age of Mauna Kea lava flows cored in the Hilo hole range in age from <200 ka to about 400 ka based on 40Ar/39Ar incremental heating and K-Ar analyses of 16 groundmass samples and one coexisting plagioclase.