Items where authors include "Agostini, S"

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Number of items: 7.

Article

Iveson, AA, Humphreys, MCS, Jenner, FE et al. (9 more authors) (2022) Tracing Volatiles, Halogens, and Chalcophile Metals during Melt Evolution at the Tolbachik Monogenetic Field, Kamchatka. Journal of Petrology, 63 (9). egac087. ISSN 0022-3530

Wu, S, Yang, Y, Jochum, KP et al. (41 more authors) (2021) Isotopic Compositions (Li‐B‐Si‐O‐Mg‐Sr‐Nd‐Hf‐Pb) and Fe 2+ /ΣFe Ratios of Three Synthetic Andesite Glass Reference Materials (ARM‐1, ARM‐2, ARM‐3). Geostandards and Geoanalytical Research. ggr.12399. ISSN 1639-4488

Iveson, AA, Humphreys, MCS, Savov, IP orcid.org/0000-0003-4218-4365 et al. (11 more authors) (2021) Deciphering variable mantle sources and hydrous inputs to arc magmas in Kamchatka. Earth and Planetary Science Letters, 562. 116848. ISSN 0012-821X

Sugden, PJ, Savov, IP orcid.org/0000-0003-4218-4365, Agostini, S et al. (3 more authors) (2020) Boron isotope insights into the origin of subduction signatures in continent-continent collision zone volcanism. Earth and Planetary Science Letters, 538. 116207. ISSN 0012-821X

McCaig, AM orcid.org/0000-0001-7416-4911, Titarenko, SS orcid.org/0000-0002-4453-0180, Savov, IP orcid.org/0000-0003-4218-4365 et al. (4 more authors) (2018) No significant boron in the hydrated mantle of most subducting slabs. Nature Communications, 9. 4602. ISSN 2041-1723

Harvey, J, Garrido, C, Savov, IP et al. (5 more authors) (2014) 11B-rich fluids in subduction zones: the role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle. Chemical Geology, 376. 20 - 30. ISSN 0009-2541

Harvey, J orcid.org/0000-0002-0390-3438, Savov, IP orcid.org/0000-0003-4218-4365, Agostini, S et al. (2 more authors) (2014) Si-metasomatism in serpentinized peridotite: The effects of talc-alteration on strontium and boron isotopes in abyssal serpentinites from Hole 1268a, ODP Leg 209. Geochimica et Cosmochimica Acta, 126. pp. 30-48. ISSN 0016-7037

This list was generated on Sat Apr 20 03:37:49 2024 BST.