XRF and ICP-MS data obtained on whole rock samples of core (obtained via drilling on IODP Expedition 350 at Site U1437, Izu-Bonin rear-arc; Igneous Unit 1) and dredged rhyolites from the surrounding area (obtained via dredging using the R/V Moana Wave in 1995, see Hochstaedter et al., 2000).
How to cite this dataset:
Heywood, L., DeBari, S., Gill, J., Straub, S., Schindlbeck-Belo, J., Escobar-Burciaga, R., Woodhead, J. 2020. Whole rock major and trace element analyses of tephras from IODP Site U1437 and dredged rocks from the surrounding area, Izu-Bonin rear-arc, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/111455.
Heywood, L.J., DeBari, S.M., Gill, J.B., Straub, S.M., Schindlbeck‐Belo, J.C., Escobar‐Burciaga, R.D. and Woodhead, J., 2020. Across‐Arc Diversity in Rhyolites From an Intra‐oceanic Arc: Evidence From IODP Site U1437, Izu‐Bonin Rear Arc, and Surrounding Area. Geochemistry, Geophysics, Geosystems, 21(2), p.e2019GC008353.
User Contributed Keyword(s):
subduction zone, tephras, rhyolites, rear-arc magmatism