The Wandashan metallogenic belt in the eastern Heilongjiang Province is a part of the giant circum-Pacific metallogenic belt. The No.258 Hill gold deposit is located at the junction of the Wandashan eugeosyncline and the Sanjiang fault basin, and is one of the most promising magmatic hydrothermal deposits at the northern Wandashan precious and polymetallic metallogenic belt (Mao et al, 2003;Huang, 2010; Qi, 2005; Li, 2011; Xue, 2012).The exposed strata in the No.258 Hill gold deposit consist mainly of Upper Triassic Dajiahe Formation and Lower Jurassic Dalingqiao Formation. The Mesozoic Hamahe granite is the largest intrusions in the mining area and is the host of the gold deposit. In addition, there are numerous stocks of dikes ranging in composition from diorite, diorite porphyrite and gabbro, locally intruding the Hamahe granite. Gold mineralization mainly occurred in the Hamahe granite and altered diorite porphyrite. Previous studies suggest that a close relationship between gold mineralization and the Mesozoic magmatism. The area is marked by numerous NE-directed folds, NW-and NE-direction faults. The NE-striking structure is the most important host structure, which controlled the location and occurrence of the orebodies.The No.258 Hill gold deposit, consists of auriferous quartz veins and sulfide disseminations in hydrothermally altered rocks. The deposit consists of 25 ore bodies that formed four mineralized blocks ranging in length from 100 to 260 m and in width from 20 to 200 m. These ore bodies are parallel to the diorite porphyrite emplaced along the NE-trending fracture, and mostly dip towards NE with a steep angle of > 85°. These ore bodies are roughly 100 m long and 1.0-3.8 m thick with Au grade of 0.62-8.28×10 -6 (averaging 2.66×10 -6 ).Hydrothermal alteration is well developed in the deposit, dominated by silicification, pyritization, sercitization, kaolinization, choloritization and carbonatization. The gold orebodies mainly occur within the zone of silicification, pyritization and sercitization. Geochronology and Geochemistry SamplingTwo monzonitic granite samples of the Hamahe granite (258-N-001 and 258-N-002) and one diorite porphyrite sample (258-N-003) were collected for zircon separation. Seven monzonitic granite and five diorite porphyrite samples were collected from exploratory trenches and drill cores of the No.258 Hill gold deposit for whole-rock geochemistry analyses. U-Pb zircon datingLA-ICP-MS Zircon U-Pb dating was used to determine the emplacement ages of the monzonitic granite and diorite porphyrite. These ages also provide good constraints on the time of gold mineralization as the intrusive rocks are closely associated with the No.258 Hill gold deposit. The monzonitic granite samples yield concordant U-Pb ages of 122.05 ± 0.72 Ma (258-N-001) and 118.01 ± 0.94 Ma (258-N-002), whereas the diorite porphyrite sample has a U-Pb age of 119.50 ± 1.30 Ma (258-N-003). The results demonstrate that the monzonitic granite and diorite porphyrite were emplaced in the Early Cretaceous, rather ...

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Precambrian microcontinents represent key tectonic units in the accretionary collages of the eastern Central Asian Orogenic Belt (ECAOB), and possess a wealth of information about the geological evolution. Here, we describe newly discovered late Neoarchean amphibolite of the Huangsong Group collected from drillhole ZK4301 at the Sishanlinchang gold mining area in the Jiamusi-Khanka Block. LA-ICP-MS U-Pb dating for zircons from the amphibolite yields a weighted-mean 207 Pb/ 206 Pb age of 2539 ± 4 Ma, which can be referred to as its protolithic age. Zircons in the 2.54-Ga amphibolite show high and positive ε Hf (t) values ranging from +4.2 to +6.8 and single-stage Hf model ages (TDM1) of 2.60 to 2.68 Ga, suggesting that a depleted mantle source might have been metasomatized by fluids/melts from subducted crustal materials. The amphibolite displays low SiO 2 and alkalis, and high TFe 2 O 3 and Mg# (0.50-0.52), and is classified as a subalkaline series, medium-to high-K calc-alkaline basaltic rock. Our geochemical and geochronological data reveal that a late Archean tectono-magmatic event is preserved in the Jiamusi-Khanka Block, providing robust evidence for the existence of an Early Precambrian basement. The 2.54-Ga basaltic magmatism likely took place in an active continental margin/island arc setting.