Japan Geoscience Union Meeting 2018

Presentation information

[EE] Poster

S (Solid Earth Sciences) » S-MP Mineralogy & Petrology

[S-MP34] Oceanic and Continental Subduction Processes

Sun. May 20, 2018 10:45 AM - 12:15 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:REHMAN Ur Hafiz(Department of Earth and Environmental Sciences, Graduate School of Science and Engineering, Kagoshima University), Tatsuki Tsujimori(Tohoku University), Chin Ho Tsai

[SMP34-P05] Boron isotope systematics of forearc serpentinites: A case study
from the California Coast Ranges

*Chinatsu Yamada1, Tatsuki Tsujimori1, Jun-Ichi Kimura2, Qing Chang2 (1.Tohoku University, 2.Department of Solid Earth Geochemistry, Japan Agency for Marine-Earth Science and Technology)

Keywords:serpentine, forearc serpentinite, boron isotope, spot analysis, Franciscan Complex, LA-MC-ICPMS

Recently, Martin et al. (2016) characterized two contrasting origins of serpentinite in central Guatemala. They proposed an idea that the tectonic origin of serpentinites can be discriminated based on boron isotopic signature. In order to test the result by Martin et al. (2016), various serpentinites from the Franciscan Complex of Northern California were investigated using in-situ spot analytical technique that had newly developed by Kimura et al. (2016). The investigated twenty serpentinites include sheared serpentinite, massive serpentinite (or serpentinized peridotite), and serpentine veins cutting fresh peridotite. The occurrences of these serpentinites are classified into serpentinite lenses within Franciscan metagreywacke, blueschist-bearing serpentinite diapir, massive serpentinized peridotite body, extremely fresh peridotite body, and various serpentinites along the San Andreas Fault. We have tested both mineralogical variations (lizardite/chrysotile vs antigorite) and textural variations (pseudomorph vs non-pseudomorph). We also made a mineralogical assessment on relict mantle minerals in serpentinites. Our study found a large variation of boron isotope (δ11B) ranging from -12.0 to +24.4‰ and boron concentrations (B=3.0-239 μg/g). Our observations together with geological context support Martin et al. (2016)’s observation in central Guatemala; in other words, boron isotope is useful for tectonic discrimination of serpentinites. In this abstract, we will introduce petrologic and geochemical diversity of forearc serpentinites in California Coast Ranges, and we also present a new insight of isotope correlations among various aspects.