d37Cl values were determined for Izu Bonin arc magmas erupted 0-44 Ma in order to better understand the time-dependent processing of volatiles in subduction zones. Pristine ash-sized particles (glass,
The Trondheim Region ophiolites in the Mid-Norwegian Caledonides represent variably tectonized ophiolite fragments. We present high-precision thermal-ionization mass spectrometry and secondary-ion mas
Geological Society of London research repository2016-06-21 更新10
The Supplementary Materials include: the detailed analytical methods for mineral BSE images and micro-XRF analysis, the Supplementary Figures S1-S5, and Supplementary Tables 1-9.