Geology, geochemistry and genesis of the Eocene Lailishan Sn deposit in the Sanjiang region, SW China

摘要

The Lailishan deposit is an important tin deposit that is genetically associated with an Early Eocene biotite granite in the western Yunnan metallogenic belt in the Sanjiang region, SW China. This study reports new zircon U-Pb ages and Hf isotopic data, whole-rock elements, mica Ar-Ar age and C-H-O-S-Pb isotope for the Lailishan Sn deposit. The mineralization-related biotite granite crystallized during the Early Eocene (50.5 Ma), with its zircon epsilon Hf(t) values ranging from -11.5 to -7.6 and two-stage Hf model ages (T-Dm2) ranging from 1.60 to 1.85 Ga. The rocks are peraluminous with A/CNK values of 0.99-1.08. The granites display high Si, Al and K contents but low Mg, Fe and Ca contents. The rocks show flat chondrite-normalized REE patterns with strong Eu negative anomalies. These characteristics indicate that the magma originated from a continental crustal source. The hydrothermal muscovite exhibits an Ar-Ar plateau age of 50.4 +/- 0.2 Ma. The delta(18) and delta D values of hydrothermal quartz from the deposit range from -7.32%o to 4.01%0 and from - 124.9%0 to -87.1%o, respectively. The delta(CPDB)-C-13 and delta O-18s(smow) values of calcite range from -11.3%0 to -3.7%o and from +2.2%0 to +12.7%0, respectively. The sulfur isotopic compositions (delta(34)Sv-car) range from +3.3%0 to +8.6%0 for sulfide separates, and the lead isotopic ratios Pb-206/Pb-204, (207)pb/(204)pb and (208)pb(204) Pb range from 18.668 to 18.746, from 15.710 to 15.743 and from 39.202 to 39.295, respectively. These isotopic compositions are similar to those of magma-derived fluids, indicating that the ore-forming fluids and materials mainly originated from magmatic rocks with some input from meteoric water. This evidence suggests that the tin mineralization is closely linked to the Lailishan I-type granites. In combination with previous data, it is proposed in this study that widespread early Eocene magmatism resulted from the slab breakoff of the subducting Neo-Tethyan slab at ca. 55 Ma. (C) 2017 Elsevier Ltd. All rights reserved.