{"title":"Early miocene adakitic porphyries in the Chagai arc, Pakistan: Petrogenesis, tectonic setting and implications for porphyry Cu-Au mineralization","authors":"Xiu-Quan Miao , Chuan-Dong Xue , Xue-Ping Yang , Yun-Ying Zhang , Jian-Lin Chen","doi":"10.1016/j.lithos.2025.108023","DOIUrl":null,"url":null,"abstract":"<div><div>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 SiO<sub>2</sub> (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 (ε<sub>Hf</sub>(t) = 2.42–9.73) and mantle-like O (δ<sup>18</sup>O = 4.99–6.06 ‰) isotopic compositions of zircon grains, along with depleted Sr ((<sup>87</sup>Sr/<sup>86</sup>Sr)<sub><em>i</em></sub> = 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.</div></div>","PeriodicalId":18070,"journal":{"name":"Lithos","volume":"502 ","pages":"Article 108023"},"PeriodicalIF":2.9000,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Lithos","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0024493725000829","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
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.
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.