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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Oakhurst
Estimated thickness of granitoid rocks in the western Sierra Nevada foothills near Oakhurst, California: A hydrogeological approach Available to Purchase
Structural-metamorphic chronology in a roof pendant near Oakhurst, California: Implications for the tectonics of the western Sierra Nevada Available to Purchase
Technocomplexes and chronostratigraphy for MIS 6-1 in southern Africa Available to Purchase
Migrations of the Indus River, Pakistan, in Response to Plate Tectonic Motions Available to Purchase
The Turkey Mountain Lime Pools, Oklahoma Available to Purchase
Inorganic Origin of Petroleum: Reply Available to Purchase
The Fine Gold Intrusive Suite: The roles of basement terranes and magma source development in the Early Cretaceous Sierra Nevada batholith Open Access
Geologic Age of the Modelo Formation, California Available to Purchase
Detrital zircon provenance and depositional links of Mesozoic Sierra Nevada intra-arc strata Open Access
DEVITOITE, A NEW HETEROPHYLLOSILICATE MINERAL WITH ASTROPHYLLITE-LIKE LAYERS FROM EASTERN FRESNO COUNTY, CALIFORNIA Available to Purchase
Day 2: The Fine Gold Intrusive Suite— Records of the nascent Cretaceous arc Available to Purchase
Abstract Today’s trip introduces Field Forum participants to the earliest stages of magmatism in the Cretaceous section of the Sierran arc. Despite the paucity of fresh rock exposed in the western foothills, we have determined that the Fine Gold Intrusive Suite is a massive (>3100 km 2 ) and long-lived (ca. 19 million years, Lackey et al., 2012) intrusive complex, preserving a record of magmatism that provides considerable insight into the evolution of arc magma systems intruding across major crustal terrane boundaries. The primary units of the Fine Gold Intrusive Suite that will be viewed during the field excursion include the Bass Lake Tonalite, Ward Mountain Trondhjemite, and Knowles Granodiorite ( Fig. 2-1 ). The low-K 2 O, 87Sr/86Sr, high-Sr/Y, high- ?18O, and peraluminous composition of the Fine Gold Intrusive Suite rocks are geochemically distinct from the younger rocks of the central and eastern Sierra (Fig. 2-2 )…