Geology, alteration, mineralization and magmatic evolution of the Southeast Zone (Cu-Mo) and Deerhorn (Cu-Au) porphyry deposits, Woodjam, central British Columbia, Canada
The Woodjam district is part of the porphyry deposits of Late Triassic to Middle Jurassic age (216–183 Ma) located in the Quesnel terrane in central British Columbia. Porphyry centers include the large Cu-Mo Southeast Zone (SEZ), hosted in the calc-alkalic Takomkane batholith, and the Au-Cu Deerhorn...
Main Author: | del Real Contreras, Irene |
---|---|
Language: | English |
Published: |
University of British Columbia
2015
|
Online Access: | http://hdl.handle.net/2429/52173 |
Similar Items
-
The Protracted Magmatism and Hydrothermal Activity Associated with the Gibraltar Porphyry Cu-Mo Deposit, South Central British Columbia, Canada.
by: Kobylinski, Christopher
Published: (2019) -
Geological characteristics and genesis of the Kemess North porphyry Au-Cu-Mo deposit , Toodoggone district, north-central British Columbia, Canada
by: McKinley, Bradley Scott Mason
Published: (2008) -
Geological characteristics and genesis of the Kemess North porphyry Au-Cu-Mo deposit , Toodoggone district, north-central British Columbia, Canada
by: McKinley, Bradley Scott Mason
Published: (2008) -
Geological characteristics and genesis of the Kemess North porphyry Au-Cu-Mo deposit , Toodoggone district, north-central British Columbia, Canada
by: McKinley, Bradley Scott Mason
Published: (2008) -
Variation in hydrothermal muscovite and chlorite composition in the Highland Valley porphyry Cu-Mo district, British Columbia, Canada
by: Alva Jimenez, Tatiana Romy
Published: (2011)