Updated Izu sample geochemical analysis compilation

Gill, James B; ORCID: 0000-0003-2584-9687; SCOPUS: 55535845900
This dataset is an updated version of Gill, 2019 (https://doi.org/10.1594/IEDA/111181). It contains published and previously unpublished XRF and ICP-MS analyses from the University California Santa Cruz (UCSC) for rock samples dredged from, and mostly behind, the Izu (Japan) volcanic front from 30° to 31°N, or from and behind Torishima to Aogashima. Most were dredged using the R/V Moana Wave in 1995. Additional data for samples from these dredges are provided in publications by Ishizuka, Machida, and Haragichi. A new distinction is made between Rift- and Rear Arc Seamount Chain-types. It relies on trace element and isotope geochemistry and supersedes the distinction between Active Rifts, Back Arc Knolls, and Western Seamounts. Samples are being archived at The University of Rhode Island- Graduate School of Oceanography. They will be available to anyone by application to URI (Kelley Group http://www.gso.uri.edu/kelley/Welcome.html).
How to cite this dataset:
Gill, J. B., 2021. Updated Izu sample geochemical analysis compilation, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111991. Accessed 2024-07-17.
DOI Creation Date:
A. Hochstaedter, J. Gill, M. Kusakabe, S. Newman, M. Pringle, B. Taylor and P. Fryer. (1990), Volcanism in the Sumisu Rift I: major element, volatile, and stable isotope geochemistry. Earth Planet. Sci. Lett. 100, 179-194. doi:10.1016/0012-821X(90)90184-Y

A. Hochstaedter, J. Gill and J. Morris. (1990), Volcanism in the Sumisu Rift II: subduction and non-subduction related components. Earth Planet. Sci. Lett. 100, 195-209. doi: 10.1016/0012-821X(90)90185-Z

A.G.. Hochstaedter, J. Gill, B. Taylor, O. Ishikuka, M. Yuasa, and S. Morita. (2000), Across-arc geochemical trends in the Izu-Bonin arc: constraints on source composition and mentle melting. J. Geophys. Res. 105, 495-512., doi:10.1029/1999JB900125

A. G. Hochstaedter, J. Gill, R. Peters, P. Broughton, P. Holden, and B. Taylor (2001), Across-arc geochemical trends in the Izu-Bonin arc: contributions from the subducting slab. Geophysics, Geochemistry, Geosystems, doi:10.1029/2000GC000105

O. Ishizuka et al. (2003) Fluid-mantle interaction in an intra-oceanic arcs… Earth and Planetary Science Letters, 211, 221-236. doi:10.1016/S0012-821X(03)00201-2

O. Ishizuka et al. (2006) Variation in the mantle sources of the northern Izu arc… J. Volc. Geothermal Res. 156, 266-290. doi:10.1016/j.jvolgeores.2006.03.005

S. Machida and Ishii T. (2003) Backarc volcanism along the en-echelon seamounts: The Enpo seasmount chain in the northern Izu-Ogasawara arc, Geochem. Geophys. Geosyt 4(8), 9006, doi:10.1029/2003GC000554

S. Machida et al. (2008) Petrology and geochemistry of cross-chains in the Izu-Bonin back arc... Geochem. Geophys. Geosyt 9(5), Q05002, doi:10.1029/2007GC001641

D. Tollstrup, J. Gill, A. Kent, D. Prinkey, R. Williams, Y. Tamura, O. Ishizuka. (2010), Across-arc geochemical trends in the Izu-Bonin arc: contributions from the subducted slab, revisited. Geochem. Geophys. Geosyst., 11, Q01X10, doi:10.1029/2009GC002847

S. Haraguchi, J-I. Kimura, R. Senda, K. Fujinaga. K. Nakamura, Y. Takaya, T. Ishii (2017) Origin of felsic volcanism in the Izu arc intra-arc rift. Contrib. Mineral. Petrol. 172, 1-25. doi:10.1007/s00410-017-1345-1

J. Gill, R. Hiscott, and Ph. Vidal (1994) Turbidite geochemistry and evolution of the Izu-Bonin arc and continents. Lithos 33, 135-168. doi:10.1016/0024-4937(94)90058-2

J. Gill et al. (2018) Tuffaceous mud is a volumetrically important volcaniclastic facies of submarine arc volcanism and record of climate change. Geochemistry, Geophysics, Geosystems 19, 1-27. doi:10.1002/2017GC007300
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Funding source(s):
National Science Foundation: 9402984
National Science Foundation: 0325189
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Izu-Bonin-Mariana Arc
User Contributed Keyword(s):
R/V Moana Wave
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