首页> 外文期刊>Mineralium Deposita >U–Pb, Re–Os, and 40Ar/39Ar geochronology of the Nambija Au-skarn and Pangui porphyry Cu deposits, Ecuador: implications for the Jurassic metallogenic belt of the Northern Andes
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U–Pb, Re–Os, and 40Ar/39Ar geochronology of the Nambija Au-skarn and Pangui porphyry Cu deposits, Ecuador: implications for the Jurassic metallogenic belt of the Northern Andes

机译:厄瓜多尔Nambija Au-skarn和Pangui斑岩铜矿床的U–Pb,Re–Os和 40 Ar / 39 Ar地质年代学:对该地区侏罗纪成矿带的影响北安第斯山脉

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New U–Pb, Re–Os, and 40Ar/39Ar dates are presented for magmatic and hydrothermal mineral phases in skarn- and porphyry-related ores from the Nambija and Pangui districts of the Subandean zone, southeastern Ecuador. Nambija has been one of the main gold-producing centers of Ecuador since the 1980s due to exceptionally high-grade ores (average 15 g/t, but frequently up to 300 g/t Au). Pangui is a recently discovered porphyry Cu–Mo district. The geology of the Subandean zone in southeastern Ecuador is dominated by the I-type, subduction-related, Jurassic Zamora batholith, which intrudes Triassic volcanosedimentary rocks. The Zamora batholith is in turn cut by porphyritic stocks, which are commonly associated with skarn formation and/or porphyry-style mineralization. High precision U–Pb and Re–Os ages for porphyritic stocks (U–Pb, zircon), associated prograde skarn (U–Pb, hydrothermal titanite), and retrograde stage skarn (Re–Os, molybdenite from veins postdating gold deposition) of the Nambija district are all indistinguishable from each other within error (145 Ma) and indicate a Late Jurassic age for the gold mineralization. Previously, gold mineralization at Nambija was considered to be Early Tertiary based on K–Ar ages obtained on various hydrothermal minerals. The new Jurassic age for the Nambija district is slightly younger than the 40Ar/39Ar and Re–Os ages for magmatic–hydrothermal minerals from the Pangui district, which range between 157 and 152 Ma. Mineralization at Nambija and Pangui is associated with porphyritic stocks that represent the last known episodes of a long-lived Jurassic arc magmatism (∼190 to 145 Ma). A Jurassic age for mineralization at Nambija and Pangui suggests that the Northern Andean Jurassic metallogenic belt, which starts in Colombia at 3° N, extends down to 5° S in Ecuador. It also adds a new mineralization style (Au-skarn) to the metal endowment of this belt. Keywords U–Pb - Re–Os - Ar–Ar - Geochronology - Ecuador - Nambija - Pangui - Skarn - Porphyry Cu - Gold Editorial handling: B. Lehmann
机译:给出了南比亚贾邦和矽卡岩与斑岩相关矿石中岩浆和热液矿物相的新的U-Pb,Re-Os和 40 Ar / 39 Ar日期。厄瓜多尔东南部Subandean区的Pangui区。自1980年代以来,南比雅一直是厄瓜多尔的主要黄金生产中心之一,归因于其高品位矿石(平均15克/吨,但经常高达300克/吨金)。盘归是最近发现的斑岩铜钼区。厄瓜多尔东南部的苏巴第斯山脉带的地质以俯冲相关的I型侏罗纪Zamora岩床为主,它侵入了三叠纪火山沉积岩。 Zamora岩床又被斑岩性储层切割,这通常与矽卡岩形成和/或斑岩型矿化有关。斑岩性储层(U–Pb,锆石),相关的前生矽卡岩(U–Pb,热液钛矿)和逆行阶段矽卡岩(Re–Os,在金沉积后的脉中的辉钼矿)的高精度U–Pb和Re–Os年龄Nambija地区在误差(145 Ma)内彼此无法区分,并且指示金矿化的侏罗纪晚期。以前,根据从各种热液矿物中获得的K–Ar年龄,Nambija的金矿化被认为是第三纪。 Nambija地区的新侏罗纪年龄比Pangui地区岩浆热液矿物的 40 Ar / 39 Ar和Re-Os年龄稍小,范围介于157和152马。 Nambija和Pangui的矿化与斑状储层有关,这些斑状储层代表着长久的侏罗纪弧岩浆作用(约190至145 Ma)的最后一次已知事件。 Nambija和Pangui的侏罗纪成矿时代表明,北安第斯侏罗纪成矿带始于哥伦比亚,南北3°,延伸至厄瓜多尔的南北5°。它还为该带的金属end赋增加了新的矿化样式(Au-skarn)。关键字U–Pb-Re–Os-Ar–Ar-年代学-厄瓜多尔-Nambija-Pangui-Skarn-斑岩铜-金编辑处理:B. Lehmann

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