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The Gibraltar porphyry-Cu deposit in the Quesnel Terrane in south-central British Columbia is hosted by the Late Triassic to Early Jurassic Granite Mountain Batholith (GMB). The GMB has been classified into four phases of tonalitic rocks with minor quartz diorite. The rocks of the Mine Phase, host of the Cu mineralization, are foliated tonalite and are extensively altered to form K-feldspar, white mica, epidote and pyrite. All zircon grains examined from the GMB are magmatic with Th/U ranging from 0.15 to 1.44 and low Nd/Yb ratios below 0.01. U-Pb dating of zircons reveals three Cumineralized intrusions within the Mine Phase ranging from 201 to 218 Ma. The age gaps between the mineralized intrusions are larger than the uncertainty of the age data. Zircons from the oldest Cumineralized intrusion (218.9±3.1 Ma) in the Mine Phase record the highest Ce4+/Ce3+ (680± 180 (1 σ), n=14). Zircons from the two other groups of Cu-mineralized intrusions in the Mine Phase show lower Ce4 +/Ce3+ (214± 64 (1σ), n=43) and those from the unmineralized Border and Granite Mountain phases of the GMB show even lower Ce4+/Ce3+ (128± 35 (1σ), n=108). Zircons from the Cretaceous Sheridan Creek Stock, south of the GMB, show low Ce4+/Ce3+ (203± 60 (1σ), n=28). The data suggest multiple pulses of intrusions and mineralization in the Mine Phase, which is supported by Re-Os ages of molybdenite which are similar to the second and third pulses of intrusions. Ages and Ce4+/Ce3+ values for zircons from Cumineralized rocks in the Mine Phase are similar to the values for intrusions associated with the Highland Valley porphyry Cu deposit in the Guichon Creek Batholith. The ratios Ce/Nd and Ce/Ce* from the measured concentrations of Ce, Nd, and Sm correlate well with Ce4+/Ce3+, based on the compositions of zircon and bulk rocks. This suggests that the compositions of detrital zircons in glacial sediments and streams may be used in mineral exploration to detect intrusions with affinity to host porphyry Cu

High cerium anomalies in zircon from intrusions associated with porphyry copper mineralization in the Gibraltar deposit, south-central British Columbia