13.07.2015 Views

Physical Volcanology, Hydrothermal Alteration and Massive ...

Physical Volcanology, Hydrothermal Alteration and Massive ...

Physical Volcanology, Hydrothermal Alteration and Massive ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

This spectacular volcanic breccia is composed of 30-60% subangular to angular,1-35 cm diameter light grey felsic volcanic fragments which contain 1-5% 1 mm quartzphenocrysts. These fragments are alligned parellel to one another, <strong>and</strong> in many places,appear as if they can be placed back together with adjacent fragments. Rare sulfide-richfragments <strong>and</strong> iron-carbonate-rich fragments (pumice) up to 5 cm in diameter can also beobserved. The matrix of this rock is composed of fine grained quartz, iron-chlorite, ironcarbonate,<strong>and</strong> sericite.In thin section, the felsic lithic fragments from this outcrop are composed ofspherulitic quartz- <strong>and</strong> K-spar(?)-phyric lava. We believe that this breccia represents aproximal dome collapse breccia or block <strong>and</strong> ash flow deposit formed from a Middle "L"lava dome that may have been located to the east near the wall of the caldera. A late faultzone located along the northeastern margin of the Sturgeon Lake ore deposit precludesobservation of the "L" stratigraphy north <strong>and</strong> east of this fault.34

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!