GRAVITY, MAGNETOTELLURIC, AND MAGNETIC FIELD DATA DISTINGUISH MAGMATIC FEATURES IN THE ILIAMNA-LAKE CLARK REGION NEAR THE PEBBLE PORPHYRY DEPOSIT
Drill cores provide samples of a suite of rock types including mostly Cretaceous granodiorites, monzonite and monzodiorites, Tertiary basalts, and a variety of sedimentary and meta-sedimentary rocks. The densities of the more felsic rocks are generally comparable to those of surrounding sediments, but lower than those of the mafic materials. In contrast, magnetic susceptibilities of the felsic and mafic samples lie within comparable ranges. A notable exception is within the Pebble deposit, where susceptibilities of ore-hosting granodiorites are much lower than those of the surrounding areas.
A ~40 x 50 km region of high magnetic anomalies representing both Cretaceous and Tertiary felsic and mafic rocks characterizes the region. Using MT data to distinguish more resistive igneous rocks from surrounding sedimentary rocks, and gravity data to distinguish felsic from mafic rocks, we model several 5-10 km wide felsic intrusions extending to ~2-4 km depth, with the greatest concentration of such intrusions occurring near the Pebble deposit. These models also suggest the presence of a few similarly scaled mafic intrusions, but most mafic bodies appear to be less than 1 km thick. The granodiorite hosting the Pebble deposit is characterized by lower resistivity and magnetic susceptibility, with the latter expressed in magnetic field derivative maps. We attribute this difference in geophysical character to hydrothermal alteration associated with formation of the deposit.