Sonia Tonarini

TL;DR: The Istituto di Geoscienze e Georisorse (IGG), with the support of the International Atomic Energy Agency (IAEA), undertook the collection, preparation and distribution of eight geological materials intended for a blind interlaboratory comparison of measurements of boron isotopic composition and concentration as mentioned in this paper.

TL;DR: In this article, the Western Anatolia Miocene-to-Present Day magmatism evolved from calc-alkaline and shoshonitic rocks (21−16 Ma) to lamproites (16−14 Ma), and eventually into OIB-type magmas (2−0 Ma) represented by the Kula volcanics.

TL;DR: In this article, B and Li isotopic data are presented for well-characterized basalts from a transect across the Cascades volcanic arc, S. Washington, for a sediment core on the incoming Juan de Fuca plate, and for dacites from Mt. St. Helens.

TL;DR: In this paper, the authors investigated the role of mafic K-andesites in the genesis of the Elba magmatism of the Tuscan Archipelago and the Italian mainland.

TL;DR: The Istituto di Geoscienze e Georisorse (IGG), on behalf and with the support of the International Atomic Energy Agency (IAEA), prepared eight geological materials (three natural waters and five rocks and minerals), intended for a blind interlaboratory comparison of measurements of boron isotopic composition and concentration as discussed by the authors.