Microgranular enclaves in island-arc andesites: A possible link between known epithermal Au and potential porphyry Cu–Au deposits in the Tulasu ore cluster, western Tianshan, Xinjiang, China

• Published in: Journal of Asian earth sciences Vol. 85; pp. 210 - 223
• Main Authors: Zhao, Xiaobo, Xue, Chunji, Symons, David T.A., Zhang, Zhaochong, Wang, Honggang
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.05.2014
• Subjects: Exploration target for porphyry Cu–Au deposit; Microgranular enclaves; Tawuerbieke; Tianshan; Tulasu ore cluster; Western China; Tulasu ore cluster; Western China; Microgranular enclaves; Tawuerbieke; Exploration target for porphyry Cu–Au deposit; Tianshan
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2014.01.014

•Sulfide-mineralized enclaves were found in andesite of the Tulasu epithermal gold ore cluster.•Both andesite and enclaves were generated from the same island-arc magma.•There is potential to find porphyry Cu–Au deposits at depth of the Tulasu basin. The successful exploration for porphyry copper deposit in western Tianshan, Xinjiang, faces great challenge. Tulasu basin is an important epithermal gold ore cluster in western Tianshan, which was formed in a southwest-Pacific-type island-arc setting during the late Paleozoic by the southward subduction of the North Tianshan ocean beneath the Yili plate. Porphyry Cu–Au deposits are possibly to be found at depth or adjacent to these epithermal gold deposits. Some sulfide-mineralized microgranular enclaves of monzonite porphyry and microdiorite were found in andesites of the Tawuerbieke gold district, Tulasu basin. The enclaves are randomly distributed, with generally round or subangular shape and commonly clearly defined within their host andesite, and have a chilled surrounding margin of andesite. The monzonite porphyry enclaves (MPE) exhibit porphyritic texture with the phenocrysts of plagioclase and K-feldspar. The microdiorite enclaves (MDE) are mainly composed of plagioclase and hornblende with an aplitic texture and massive structure. The host andesites show porphyritic texture, with the phenocrysts major of plagioclase, minor of hornblende and clinopyroxene. The groundmass consists of short-column plagioclase and minor clinopyroxene with a hyalopilitic texture. Zircon grains from a MPE sample yield a weighted 206Pb/238U age of 356.2±4.3Ma (n=13, MSWD=1.11), which is effectively coincident with the 360.5±3.4Ma (n=20, MSWD=0.61) of an andesite sample within analytical error, indicating that they were coeval. In addition, the MPE, MDE and the andesite samples share similar normalized incompatible element and rare earth element patterns that are characterized by a pronounced enrichment of large ion lithophile elements and a deficit of high field strength elements. Moreover, the samples show similar Nd isotope compositions to the contemporary andesites and basaltic andesites. Detailed petrology, geochronology and geochemistry studies suggest that these enclaves were captured from an underlying body during the eruption of island-arc magma. Thus, unmapped cognate porphyry intrusions associated with Cu–Au mineralization may exist under the andesite strata. This evidence in combination with the low- and high-sulfidation epithermal gold deposits, acidic hydrothermal alterations, and copper mineralization evidence, suggests that a porphyry–epithermal Cu–Au metallogenic system might occur in the Tulasu basin of western Tianshan, and that the Tawuerbieke district should be an important target for porphyry Cu–Au exploration.