Timing of formation of the Keketale Pb–Zn deposit, Xinjiang, Northwest China, Central Asian Orogenic Belt: Implications for the metallogeny of the South Altay Orogenic Belt

Abstract

The Keketale is the largest Pb–Zn deposit in the volcano‐sedimentary Maizi Basin of the South Altay Orogenic Belt (AOB), Northwest China. The stratabound orebodies are hosted in a suite of meta‐sedimentary rocks intercalated with volcanic rocks of the Lower Devonian Kangbutiebao Formation. The massive and banded ores representing the main mineralization stage are relatively well‐preserved in the ore district. This paper reports systematic geochronological results including the zircon laser ablation–multiple collector–inductively coupled plasma–mass spectrometry (LA‐MC‐ICP‐MS) U–Pb analyses on two meta‐felsic volcanic rocks from the Kangbutiebao Formation and Rb–Sr isotope dating on seven sphalerite samples from the main mineralization stage, together with some sulphur isotopic data to constrain the mineralization age and the genesis of the deposit. Rb–Sr isotope dating yield an isochron age of 398.2 ± 3.3 Ma generally synchronous with the zircon (LA‐MC‐ICP‐MS) U–Pb analyses of a meta‐rhyolite and a meta‐dacite from the strata (410.5 ± 1.3 Ma and 394.8 ± 1.9 Ma, respectively). The δ34S values of seven pyrite samples in the main massive and banded ores vary from −12.4‰ to −6.2‰, indicating that the main ore‐forming sulphur of the deposit was derived from bacterial reduction of seawater sulphate. By integrating the field, chronological, and isotopic evidences, we conclude that the Keketale Pb–Zn deposit is a VMS‐type deposit. Combining our results with the isotopic geochronology in the South AOB, we argue that the South AOB has undergone three mineralization episodes: the syndepositional mineralization (412–387 Ma), the subvolcanic hydrothermal‐related mineralization (382–379 Ma), and the epigenetic mineralization that is genetically linked to regional metamorphism and deformation (260–204 Ma). The Keketale Pb–Zn deposit is a product of the Devonian seafloor hydrothermal exhalation system in the South AOB.

Petrogenesis of Devonian and Permian Pegmatites in the Chinese Altay: Insights into the Closure of the Irtysh–Zaisan Ocean

“…The dating data show that ages of samples from the Habahe Group mostly range from Cambrian to Ordovician, whereas for the Habahe/Kulumuti Formation, these vary from Neoproterozoic to Silurian [35,37,38,118,119]. Unit 3 (Qiongkuer Terrance) comprises the Early Devonian Kangbutiebao and Middle Devonian Altay formations as well as the Cambrian-Ordovician Habahe Group [35,38,84,[120][121][122][123][124][125][126][127][128][129][130]. Therefore, the Permian Jiamanhaba pegmatite was most likely derived from the partial melting of sedimentary/metasedimentary rocks of the Kangbutiebao Formation in the northwest of the Qiongkuer Terrance, and minor mantle-derived or juvenile materials were added to the original magma.…”

Spermatophyta (Plantae) and invasive alien plants of Wanda Mountains in China: a first checklist

“…The main vein of Wanda Mountains runs from northeast to southwest, extending from Raoli River in the northwest to Wusuli River in the east and then to Guokui Mountain in the south. It is the watershed between Raoli River and Muling River, about 350 km long from east to west and 250 km wide from north to south ( Yang and Yang 2017 ). The Wanda Mountains are low mountain and hilly areas with an altitude of 300 ~ 500 m and an average gradient of 10° ~ 15° ( Guo et al 2008 ).…”