U-Pb Ages of Intrusive Rocks and Ar/Ar Plateau Ages of Copper-Gold- Silver Mineralization Associated with Alkaline Intrusive Centres at Mount Polley and the Iron Mask Batholith, Southern and Central British Columbia
نویسندگان
چکیده
Por phyry de pos its in Brit ish Co lum bia have pro duced more than $27 bil lion worth of cop per and gold. They formed dur ing two dis tinct pe ri ods in the de vel op ment of the Cor dil lera: the first in the Late Tri as sic to Early Ju ras sic and the sec ond in the Cre ta ceous to Eocene. Most por phyry pro duc tion has come from the south ern part of Quesnel Terrane, where two cy cles of calcalkaline through al ka line magmatism are rec og nized in the Late Tri as sic and Early Ju ras sic. The rea son for the ca. 10 Ma cy cle of early calcalkaline and later al ka line vol ca nism, plutonism and min er al iza tion is not fully re solved, but the same pat tern re peated in the cen tral and north ern parts of the terrane sug gest a feature fundamental to the Quesnel Arc genesis.
منابع مشابه
زمینشناسی، کانیسازی، دگرسانی و دستاوردهای ژئوشیمیایی در منطقه کجه فردوس
The study area is situated within the Lut Block 50 Km northeast of Ferdows. The oldest exposed rocks are Cretaceous limestone. Kerman conglomerate cover the limestone. Dacite-rhyodacite lava and pyroclastic rocks erupted over Kerman conglomerate. Volcanic activities took place at different time in Tertiary. The composition ranges between trachyandesite, andesite, andesite-basalt and rhyolitic ...
متن کاملGEOLOGY AND U-Pb GEOCHRONOLOGY OF INTRUSIVE ROCKS ASSOCIATED WITH MINERALIZATION IN THE NORTHERN TAHTSA LAKE DISTRICT, WEST-CENTRAL BRITISH COLUMBIA
The Bulkley Suite of intrusions are spatially associated with numerous important mineral occurrences in westcentral British Columbia. Previous K-Ar dating studies indicated that the Bulkley Suite ranges in age from 70 to 84 Ma (Carter, 1981). The purpose of this study is to better constrain the timing of Bulkley Suite magmatism and associated mineralization in the northern Tahtsa Lake District....
متن کاملField Constraints on Diverse Igneous Processe:~ in the Iron Mask Batholith
The Iron Mask batholith is an Early Jurassic composite alkaline intrusion located southwest of Kamloops in southcentral British Columbia (Figure 2-6-l). It lies in the southern portion of the Quesnel trough in the lntermontane tcctonic belt. It is a northwest-trending body approximately 22 kilomctres long and 5 kilometres wide intruding volcanic and sedimentary rocks of the eastern belt of the ...
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Silver Queen mint in central British Columbia, is located approximately 35 kilometres south of Houston and 3 kilometres east of 0wt.n Lake (Figure 2-7-1). Although currently inactive, it was worked briefly in the early 1970s for gold. silver, copper, zinc, lead and cadmium. The deposit is hosted by Cretaceous rocks of the informal Tip Top Hill group (78.322.67 Ma, K-Ar whole rock), with the age...
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