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| 1 | Fluid Inclusion and H-O Isotope Geochemistry of the Phapon Gold Deposit, NW Laos: Implications for Fluid Source and Ore Genesis显示文摘The Phapon gold deposit, located in northern Laos, is a unique large-scale gold deposit in Luang Prabang-Loei metallogenic belt. It is hosted in the Lower Permian limestone and controlled by a NE-trending ductile-brittle fault system. There are three types of primary ore including auriferous calcite vein type, disseminated type, and breccia type, and the first two are important in the Phapon gold deposit. Based on fluid inclusion petrography and microthermometry, three types of primary fluid inclusions including type 1 liquid-rich aqueous, type 2 vapor-rich aqueous and type 3 daughter mineralbearing aqueous were identified in hydrothermal calcite grains. The ore-forming fluids are normally homogeneous, as indicated by the widespread type 1 inclusions with identical composition. The coexistence of type 1 and type 2 inclusions, showing similar final homogenization temperature but different compositions, indicate that fluid immiscibility did locally take place in both two types of ores. The results of microthermometry and H-O isotopes geochemistry indicate that there are little differences on ore-fluid geochemistry between the auriferous calcite vein-type and disseminated type ores. The oreforming fluids are characterized by medium-low temperatures(157–268 oC) and low salinity(1.6 wt.%–9.9 wt.% NaCl eq.). It is likely to have a metamorphic-dominant mixed source, which could be associated with dehydration and decarbonisation of Lower Permian limestone and Middle–Upper Triassic sandstones during the dynamic metamorphism. The fluid-wallrock interaction played a major role, and the locally occurred fluid-immiscible processes played a subordinate role in gold precipitation. Combined with the regional and ore deposit geology, and ore-fluid geochemistry, we suggest that the Phapon gold deposit is best considered to be a member of the epizonal orogenic deposit class. | Linnan Guo Shusheng Liu Lin Hou Jieting Wang Meifeng Shi Qiming Zhang Fei Nie Yongfei Yang Zhimin Peng | 2019 | Journal of Earth Science2019，30，1： | 11 |
| 2 | Geology, Geochronology, and Hf Isotopic Composition of the Pha Lek Fe Deposit, Northern Laos: Implications for Early Permian Subduction-Related Skarn Fe Mineralization in the Truong Son Belt显示文摘The Truong Son metallogenic belt in central Laos and Vietnam is an important Fe-Cu-Sn-Au polymetallic ore district. The Pha Lek Fe deposit is closely related to Late Carboniferous– Early Permian I-type granitic magmatism, and contains >50 Mt @ 45% to 50% of Fe ore. Ore minerals occur mainly as magnetite and hematite in the skarn alteration zone between a granitic pluton and metamorphosed Middle–Upper Devonian carbonates. The granitic pluton comprises granodiorite and granite, with zircon U-Pb dating indicating synchronous emplacement at 288.2±1.3 and 284.9±1.2 Ma, respectively. Zircons from these granitoids have ε_(Hf)(t) values of 2.9–11.2 and relatively young TDM2 ages(<1.0 Ga), indicating an origin by partial melting of depleted mafic crust or magma mixing. Previous studies have shown that these granitoids have high Y, Yb, and K_2O contents, and low Sr and Na_2O contents, which are interpreted as the melting of mafic continental crust. Pyrite of the main mineralization stage yields an ^(187)Re/^(188)Os-^(187)Os/^(188)Os isochron age of 287±17 Ma, indicating that mineralization is associated with Pha Lek granitic magmatism. A Late Carboniferous–Early Permian subduction-related skarn-type Fe mineralization model is proposed for the Pha Lek deposit. More evidence is needed to verify a hypothesis of volcanic overprinting during Late Triassic post-collisional extension. | Lin Hou Shusheng Liu Linnan Guo Fuhao Xiong Chao Li Meifeng Shi Qiming Zhang Siwei Xu Songyang Wu | 2019 | Journal of Earth Science2019，30，1： | 2 |
| 3 | An electrochemical biosensor based on DNA“nano-bridge”for amplified detection of exosomal microRNAs显示文摘Exosomal miRNAs,as potential biomarkers in liquid biopsy for cancer early diagnosis,have aroused widespread concern.Herein,an electrochemical biosensor based on DNA“nano-bridge”was designed and applied to detect exosomal microRNA-21(miR-21)derived from breast cancer cells.In brief,the target miR-21 can specifically open the hairpin probe 1(HP1)labeled on the gold electrode(GE)surface through strand displacement reaction.Thus the exposed loop region of HP1 can act as an initiator sequence to activate the hybridization chain reaction(HCR)between two kinetically trapped hairpin probes:HP2 immobilized on the GE surface and biotin labeled HP3 in solution.Cascade HCR leads to the formation of DNA“nano-bridge”tethered to the GE surface with a great deal of“piers”.Upon addition of avidin-modified horseradish peroxidase(HRP),numerous HRP were bound to the formed“nano-bridge”through biotin-avidin interaction to arouse tremendous current signal.In theory,only a single miR-21 is able to trigger the continuous HCR between HP2 and HP3 until all of the HP2 are exhausted.Therefore the proposed biosensor achieved ultrahigh sensitivity toward miR-21 with the detection limit down to 168 amol/L,as well as little cross-hybridization even at the single-base-mismatched level.Successful attempts were also made in the detection of exosomal miR-21 obtained from the MCF-7 of breast cancer cell line.To our knowledge,this is the first attempt to built horizontal DNA nano-structure on the electrode surface for exosomal miRNAs detection.In a word,the high sensitivity,selectivity,low cost make the proposed method hold great potential application for early point-of-care(POC)diagnostics of cancer. | Jing Zhang Meifeng Hou Guanyu Chen Huifang Mao Wenqian Chen Wenshen Wang Jinghua Chen | 2021 | Chinese Chemical Letters2021，32，11： | 0 |
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