Fluid inclusions,C-H-O-S-Pb isotope systematics,geochronology and geochemistry of the Budunhua Cu deposit,northeast China:Implications for ore genesis

The Budunhua Cu deposit is located in the Tuquan ore-concentrated area of the southern Great Xing’an Range,NE China.This deposit includes the southern Jinjiling and northern Kongqueshan ore blocks,separated by the Budunhua granitic pluton.Cu mineralization occurs mainly as stockworks or veins in the outer contact zone between tonalite porphyry and Permian metasandstone.The ore-forming process can be divided into four stages involving stage Ⅰ quartz-pyrite-arsenopyrite;stage Ⅱ quartz-pyrite-chalcopyrite-pyrrhotite;stage Ⅲ quartz--polynetallic sulfides;and stage IV quartz-calcite.Three types of fluid inclusions(FIs) can be distinguished in the Budunhua deposit:liquid-rich two-phase aqueous FIs(L-type),vapour-rich aqueous FIs(V-type),and daughter mineral-bearing multi-phase FIs(S-type).Quartz of stages Ⅰ-Ⅲ contains all types of FIs,whereas only L-type FIs are evident in stage Ⅳ veins.The coexisting V-and S-type FIs of stages Ⅰ-Ⅲ have similar homogenization temperatures but contrasting salinities,which indicates that fluid boiling occurred.The FIs of stages Ⅰ,Ⅱ,Ⅲ,and Ⅳyield homogenization temperatures of 265-396℃,245-350℃,200-300℃,and 90-228℃ with salinities of3.4-44.3 wt.%,2.9-40.2 wt.%,1.4-38.2 wt.%,and 0.9-9.2 wt.% NaCl eqv.,respectively.Ore-forming fluids of the Budunhua deposit are characterized by high temperatures,moderate salinities,and relatively oxidizing conditions typical of an H2 O-NaCl fluid system.Mineralization in the Budunhua deposit occurred at a depth of0.3-1.5 km,with fluid boiling and mixing likely being responsible for ore precipitation.C-H-O-S-Pb isotope studies indicate a predominantly magmatic origin for the ore-forming fluids and materials.LA-ICP-MS zircon U-Pb analyses indicate that ore-forming tonalite porphyry and post-ore dioritic porphyrite were formed at 151.1±1.1 Ma and 129.9±1.9 Ma,respectively.Geochemical data imply that the primary magma of the tonalite porphyry formed through partial melting of Neoproterozoic lower crust.On the basis of available evidence,we suggest that the Budunhua deposit is a porphyry ore system that is spatially,temporally,and genetically associated with tonalite porphyry and formed in a post-collision extensional setting following closure of the Mongol-Okhotsk Ocean.

Isolation and phylogenetic analysis of feline calicivirus strains from various region of China

Feline calicivirus(FCV)is an important feline pathogen mainly causing upper respiratory tract disease,conjunctivitis,and stomatitis,and it is classifed into genotype I and genotype II.To investigate the prevalence and molecular characteristics of FCV,this study collected 337 cat swab samples from animal hospitals in diferent regions of China from 2019 to 2021.The positive detection rate of FCV was 29.9%(101/337)by RT-PCR.Statistical analysis showed that FCV prevalence was signifcantly associated with living environment(p=0.0004),age(p=0.031)and clinical symptoms(p=0.00),but not with sex(p=0.092)and breed(p=0.171).The 26 strains of FCV were isolated using F81 cells.Phylogenetic analysis showed that 10 isolates belonged to genotype I,and 16 isolates belonged to genotype II.These 26 isolates were highly genetically diverse,of which HB7 isolate had three same virulence-related amino acid loci with VSD strains.Potential loci distinguishing diferent genotypes were identifed from 26 isolates,suggesting the genetic relationship between diferent genotypes.In addition,selection pressure analysis based on capsid protein of 26 isolates revealed that the protein is under diversifying selection.This study reveals the genetic diversity of FCV and provides a reference for the screening of vaccine candidate strains and the development of vaccines with better cross-protection efects.