Early miocene adakitic porphyries in the Chagai arc, Pakistan: Petrogenesis, tectonic setting and implications for porphyry Cu-Au mineralization

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Xiu-Quan Miao , Chuan-Dong Xue , Xue-Ping Yang , Yun-Ying Zhang , Jian-Lin Chen
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引用次数: 0

Abstract

Numerous porphyry Cu-Au deposits were formed in the Chagai arc, western Pakistan, but their origin remains debated. To address this issue, we conducted zircon U-Pb dating, zircon Hf-O and plagioclase Sr isotopic analyses, and geochemical characterization of ore-bearing biotite granitic porphyries (BGP) from the Saindak area in the Chagai arc. These BGP, formed during the early Miocene (21.9–21.7 Ma), exhibit adakite-like geochemical characteristics, including high SiO2 (60.5–67.9 wt%) and low Y (6.41–9.13 ppm) contents, coupled with high Sr/Y (26.2–116) ratios. The depleted Hf (εHf(t) = 2.42–9.73) and mantle-like O (δ18O = 4.99–6.06 ‰) isotopic compositions of zircon grains, along with depleted Sr ((87Sr/86Sr)i = 0.70297–0.70482) isotopic compositions and high anorthite (An = 56.5–69.4 %) contents of plagioclase crystals, suggest that these BGP rocks were derived from an oceanic slab. Slab melting may cause the exceptionally high Cu (667–3060 ppm, average of 1416 ppm) contents of the studied BGP samples, which facilitates the formation of porphyry Cu-Au deposits.
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来源期刊
Lithos
Lithos 地学-地球化学与地球物理
CiteScore
6.80
自引率
11.40%
发文量
286
审稿时长
3.5 months
期刊介绍: Lithos publishes original research papers on the petrology, geochemistry and petrogenesis of igneous and metamorphic rocks. Papers on mineralogy/mineral physics related to petrology and petrogenetic problems are also welcomed.
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