Seismic structure of the crust and upper mantle in the Peace River Arch region, Canada. J. Geophys. Res., 94fB5): 5729-5744.Zelt, C. A. (1989), Seismic structure of the crust and upper mantle in the Peace River Arch region, Ph.D. Thesis, University of British Columbia, 223 pp.,...
Analysis of data at the mid-array and easternmost sites, LAS and EGM respectively, permits this zone to be mapped northeastward to a depth of 54 km beneath the British Columbia mainland, approximately 250 km from the locus of subduction.The subducting oceanic crust is imaged at...
The Upper Cretaceous carbonates along the Zagros thrust-fold belt “Harir-Safin anticlines” experienced extensive hot brine fluids that produced several phases of hydrothermal cements, including saddle dolomites. Detailed fluid inclusion microthermometr