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    Wilt Jenney 1976 Tectonic Digest AGS
    September 29, 2020
    Abbott et al 1991 Magma chemistry ore deposits field trip 8 NV
    September 29, 2020

    Keith Rasmussen 2019 Wilderness Granite Catalina Hwy Tucson AZ

    By: Magma Chem Research Institute

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    Abstract
    8-1 Keith, S.B., and Rasmussen, J.C., 2019, Wilderness Granitic Suite along Catalina Highway – petrologic and tectonic significance of the Wilderness plutonic suite: products from a massive water-flood event of hydrous crustal melting during high-speed flat subduction in the latest Laramide: Arizona Geological Society Spring Field Trip 2019, June 8, 2019, 69 p.

    Categories: Field Trip Guides, Membership Publications, Publication
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    Description

    Abstract
    8-1 Keith, S.B., and Rasmussen, J.C., 2019, Wilderness Granitic Suite along Catalina Highway – petrologic and tectonic significance of the Wilderness plutonic suite: products from a massive water-flood event of hydrous crustal melting during high-speed flat subduction in the latest Laramide: Arizona Geological Society Spring Field Trip 2019, June 8, 2019, 69 p.

    ABS

    Numerous field guides have been published on the geology of the Santa Catalina Mountains (Shakel [1978], Naruk and Bykerk-Kauffman [1999], Force [2001], and Spencer [2007]). This field trip emphasizes the peraluminous, two-mica Wilderness Granite Suite (60-34 Ma) and accompanying tectonic fabrics and cross-cutting relationships (Figure 1, Figure 2, and Figure 3). The main goal of this field trip is to demonstrate with field evidence the petrologic and tectonic connection of Wilderness Granite suite peraluminous magmatism and associated mylonitization to compressive flat subduction beneath the North American plate in the Eocene.

    STOP 1: Babad Do’ag vista overlook near base of mountain, STOP 2: Windy Point, STOP 3: Bear Wallow thrust fault, STOP 4: Garnet schlieren south of Summerhaven

    Key words
    Catalina highway, Santa Catalina Mountains, Pima County, Tucson, Peraluminous, two-mica granite, Wilderness Granite suite, Babad D’ag vista, Windy Point, Bear Wallow, Garnet schlieren, Summerhaven

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    Print to Order, Digital Version

    Product details

    Abstract
    8-1 Keith, S.B., and Rasmussen, J.C., 2019, Wilderness Granitic Suite along Catalina Highway – petrologic and tectonic significance of the Wilderness plutonic suite: products from a massive water-flood event of hydrous crustal melting during high-speed flat subduction in the latest Laramide: Arizona Geological Society Spring Field Trip 2019, June 8, 2019, 69 p.

    ABS

    Numerous field guides have been published on the geology of the Santa Catalina Mountains (Shakel [1978], Naruk and Bykerk-Kauffman [1999], Force [2001], and Spencer [2007]). This field trip emphasizes the peraluminous, two-mica Wilderness Granite Suite (60-34 Ma) and accompanying tectonic fabrics and cross-cutting relationships (Figure 1, Figure 2, and Figure 3). The main goal of this field trip is to demonstrate with field evidence the petrologic and tectonic connection of Wilderness Granite suite peraluminous magmatism and associated mylonitization to compressive flat subduction beneath the North American plate in the Eocene.

    STOP 1: Babad Do’ag vista overlook near base of mountain, STOP 2: Windy Point, STOP 3: Bear Wallow thrust fault, STOP 4: Garnet schlieren south of Summerhaven

    Key words
    Catalina highway, Santa Catalina Mountains, Pima County, Tucson, Peraluminous, two-mica granite, Wilderness Granite suite, Babad D’ag vista, Windy Point, Bear Wallow, Garnet schlieren, Summerhaven

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