Granulite Facies Metamorphism in the Coast Range Crystalline Belt

Author:

Hollister Lincoln S.

Abstract

Mineral assemblages diagnostic of the granulite facies of metamorphism occur between Terrace and Prince Rupert, British Columbia. The estimated pressure (5–8 kb) and temperature (750–850 °C) of metamorphism are important constraints in unravelling the geologic history of the Coast Range batholithic complex.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

Cited by 35 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Architecture and Evolution of the Crust during Continental Arc Magmatism: A Transect through the Coast Mountains Batholith, British Columbia;Architecture and Evolution of the Crust during Continental Arc Magmatism: A Transect through the Coast Mountains Batholith, British Columbia;2020-07-08

2. Sediment underthrusting within a continental magmatic arc: Coast Mountains batholith, British Columbia;Tectonics;2017-10

3. Mid-Cretaceous–Recent crustal evolution in the central Coast orogen, British Columbia and southeastern Alaska;Crustal Cross Sections from the Western North American Cordillera and Elsewhere: Implications for Tectonic and Petrologic Processes;2009

4. Granulites of the Kolpakovskaya Series in the sredinny range, Kamchatka: A myth or reality?;Petrology;2008-03

5. Two-stage exhumation of midcrustal arc rocks, Coast Mountains, British Columbia;Tectonics;2005-10

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