Dataset Information

Coulthard, Daniel A
Reagan, Mark K; ORCID: 0000-0003-1628-4194
Shimizu, Kenji
Bindeman, Ilya N
Brounce, Maryjo
Almeev, Renat R
Ryan, Jeffrey
Chapman, Timothy
Shervais, John
Pearce, Julian A

International Ocean Discovery Program Expedition 352 to the Bonin forearc drilled the sequence of volcanic rocks erupted in the immediate aftermath of subduction initiation along the western margin of the Pacific Plate. Pristine volcanic glasses collected during this expedition were analyzed for major and trace elements, halogens, sulfur, water, and H and O isotopes with goals of characterizing the fluids and melts of subducted materials that were involved in generating the nascent upper plate crust.

Coulthard, D. A., Reagan, M. K., Shimizu, K., Bindeman, I. N., Brounce, M., Almeev, R. R., Ryan, J., Chapman, T., Shervais, J., Pearce, J. A., 2020. Major and trace element concentrations, stable isotope ratios, and water contents for volcanic glasses from the Bonin forearc (IODP Expedition 352), Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111722. Accessed 2024-09-18.

2020-10-27

Daniel A. Coulthard Jr., Mark K. Reagan, Kenji Shimizu, Ilya N. Bindeman, Maryjo Brounce, Renat R. Almeev, Jeffrey Ryan, Timothy Chapman, John Shervais, and Julian A. Pearce, (2020), Magma source evolution following subduction initiation: Evidence from the element concentrations, stable isotope ratios, and water contents of volcanic glasses from the Bonin forearc (IODP Expedition 352), Geochemistry, Geophysics, Geosystems, accepted for publication.

Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]

National Science Foundation: OCE1558647

Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Bonin forearc, Izu-Bonin-Mariana

IODP Expedition 352, subduction initiation, forearc

2020-10-27

Dataset