The Mount Barr Plutonic Complex (MBPC) is a circular body of intrusive rock in the Cascade Mountains of southern British Columbia , Canada. It is located 19 km (12 mi) southwest of the district municipality of Hope , centered around Wahleach Lake . The complex takes its name from Mount Barr , one of many mountains consisting of MBPC intrusive rocks.
6-561: Three granitoid intrusions of Miocene age comprise the MBPC. The largest intrusion consists of rocks ranging from quartz diorite to quartz monzonite and makes up 80% of the complex. Two younger stocks are situated within the main intrusion and consist of quartz monzonite. K–Ar dating of the MBPC has given ages ranging from 21 to 16 million years old. 49°15′49″N 121°33′35″W / 49.26361°N 121.55972°W / 49.26361; -121.55972 This article about
12-575: A continental arc or by convergence yielding continental collisions. Generally, the evolution to granitoid magmas requires a thermal disturbance to ascent though continental crust. Most granitoids are generated from crustal anatexis , the partial melting of the crust; however the mantle may contribute both heat and material. Granitoids can occur coeval with volcanic rocks that have equivalent chemical composition (granite– rhyolite , syenite– trachyte , granodiorite – dacite etc.) however, these extrusive rocks are often eroded so just
18-493: A complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based on: geochemistry , modal content, emplacement depth, and tectonic regime . There are several generalizations that apply to the majority of granitoids. Typically, granitoids occur where orogeny thickens continental crust either by subduction yielding
24-628: A specific Canadian geological feature is a stub . You can help Misplaced Pages by expanding it . This article about a location in the Interior of British Columbia , Canada is a stub . You can help Misplaced Pages by expanding it . Granitoid A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz , plagioclase , and alkali feldspar . Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites . As only two of
30-416: The plutonic rocks outcrop. Granitoids can form in all tectonic environments. There are numerous exceptions to these generalizations. For example, granitoids can form in anorogenic environments , a granitoid source rock can be from the mantle (for example, at intraplate hotspots ) and the melting mechanism can be radiogenic crustal heat . This igneous rock -related article
36-454: The three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid -bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms granite and granitic rock are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give
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