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James L. Aronson

Researcher at Dartmouth College

Publications -  49
Citations -  3160

James L. Aronson is an academic researcher from Dartmouth College. The author has contributed to research in topics: Illite & Diagenesis. The author has an hindex of 29, co-authored 49 publications receiving 3018 citations. Previous affiliations of James L. Aronson include Case Western Reserve University.

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Geology, geochronology, and rift basin development in the central sector of the Main Ethiopia Rift

TL;DR: In this paper, six major volcanic episodes are recognized in the rift9s development over a time span from the late Oligocene to the Quaternary using K/Ar data.
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Late PlioceneHomoand Oldowan Tools from the Hadar Formation (Kada Hadar Member), Ethiopia

TL;DR: Rapport preliminaire de la decouverte d'un maxilaire d'Homo associe a un outillage Oldowayen et a une faune du Pliocene final dans une formation Hadar en Ethiopiaie Les elements de datation 4 0A R/3 9A R indiquent indiquant un age de 23 MA ± 007 Ils indiqueraient la plus ancienne association de restes hominides et d'outillage and probablement la plus-ancienne sequence datee du
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Late Eocene–Recent volcanism and faulting in the southern main Ethiopian rift

TL;DR: In this article, the authors used K-Ar and 40 Ar/39 Ar geochronology data from a transect of the Chamo basin and the Amaro horst-Galana basin to estimate a minimum 12 km crustal extension (β ≈ 1.12), and infer that maximum extension across the southern Ethiopian rift is less than 25 km.
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New age constraints on the timing of volcanism and tectonism in the northern Main Ethiopian Rift southern Afar transition zone (Ethiopia)

TL;DR: In this article, 40 K-Ar and 40 Ar / 39 Ar isotopic ages from the northern Main Ethiopian Rift (MER)-southern Afar transition zone provide insights into the volcano-tectonic evolution of this portion of the East African Rift system.
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Areal distribution and age of low-K, high-alumina olivine tholeiite magmatism in the northwestern Great Basin

TL;DR: In this article, the authors identify and characterize a widespread low-K, high-alumina olivine tholeiite (HAOT) magma type in the northwestern Great Basin.