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Variety and origin of magmas on Shatsky Rise, northwest Pacific Ocean

Sano, Takashi; Shimizu, Kenji; Ishikawa, Akira; Senda, Ryoko; Chang, Qing; Kimura, Jun Ichi; Widdowson, Mike; Sager, William W.

Authors

Takashi Sano

Kenji Shimizu

Akira Ishikawa

Ryoko Senda

Qing Chang

Jun Ichi Kimura

Mike Widdowson

William W. Sager



Abstract

Shatsky Rise consists of thick (∼30km maximum) basaltic crust with various geochemical compositions. Geochemistry data indicate that four magma types exist on the plateau; namely normal, low-Ti, high-Nb, and U1349 types. The normal type is the most abundant in volume and appears on all three large edifices of the plateau: Tamu, Ori, and Shirshov massifs. Composition of the normal type is similar to normal mid-ocean ridge basalt (N-MORB) composition, but with slight relative enrichment of the more incompatible elements. The low-Ti type is distinguished from the normal type basalt by slightly lower Ti content at a given MgO. Composition of the high-Nb type is characterized by distinctively high contents of incompatible trace elements. U1349 type basalts are composed of more primitive and depleted compositions compared with the others. The normal type basalts constitute ∼94% of the lava units of the oldest Tamu Massif and non-normal types (i.e., the other three types) basalts comprise ∼57% on the younger Ori Massif, implying that geochemical compositions may have become heterogeneous with time. Petrological examination demonstrates that compositions of the normal-, low-Ti-, and high-Nb-type basalts evolved through fractional crystallization of olivine, plagioclase, and augite in shallow magma chambers (

Citation

Sano, T., Shimizu, K., Ishikawa, A., Senda, R., Chang, Q., Kimura, J. I., Widdowson, M., & Sager, W. W. (2012). Variety and origin of magmas on Shatsky Rise, northwest Pacific Ocean. Geochemistry, geophysics, geosystems G³, 13(8), Article Q08010. https://doi.org/10.1029/2012GC004235

Journal Article Type Article
Acceptance Date Jul 18, 2012
Online Publication Date Aug 18, 2012
Publication Date Aug 1, 2012
Deposit Date May 27, 2022
Journal Geochemistry, Geophysics, Geosystems
Electronic ISSN 1525-2027
Publisher American Geophysical Union
Peer Reviewed Peer Reviewed
Volume 13
Issue 8
Article Number Q08010
DOI https://doi.org/10.1029/2012GC004235
Keywords Expedition 324; Integrated Ocean Drilling Program; Shatsky Rise; Chemical stratigraphy; Large igneous province; Oceanic plateau
Public URL https://hull-repository.worktribe.com/output/3566481