Tectonomagmatic Metallogenic System of Dexing Ore Field, Jiangxi, China

ore deposits and a large number of ore occurrences cluster in Dexing ore field which is 20 km long and 12 km wide. The tectonic evolution, magmatism, as well as the metallogeny are controlled by the Northeast Jiangxi deep seated fracture belt (NJDFB). The source is believed to have been derived from the Meso-Neoproterozoic marine volcanism. The magmatic activity of Mesozoic I type granite could have provided the metal elements, thermal fluid, heat, and the space for ore forming processes. A unified geological model is proposed, which combines the tectonism, magmatism and metallogeny as the basic control of the giant metal mineralizations.

METALLOGENIC ANALYSIS OF THE DEXING COPPER-GOLD-LEAD-ZINC POLYMETALLIC DEPOSITS, JIANGXI PROVINCE, CHINA

The paper discusses the tectonic setting of the fortnation of the Dexing giant copper-gold-lead-zinc deposit and its geological features and demonstrates in detail the polygenetic compound mechanism of its formation.

Isotopic tracing of ore-forming source materials for Dexing porphyry copper deposit of Jiangxi, China

Dexing copper deposit is the biggest porphyry copper deposit in China. By researching isotopes of C,Si and Cu from the samples of Tongchang and Fujiawu ore-field, the authors found that δ13CPDB values of siderite were close to the δ13CPDB value of original magma; δ30Si values of the samples at the ore-forming stage were close to the δ30Si value range of magma, δ30Si values of partial samples were far away from it; Cu isotopic compositions of massive chalcopyrite formed at the early ore-forming stage are higher than that of veinal chalcopyrite formed at the later ore-forming stage. The results show that ore-forming materials were mainly derived from the porphyry body, and part of them were from wall rock materials.

Ore Zoning and Dynamics of Ore-Forming Processes of Yinshan Polymetallic Depost in Dexing,Jiangxi

The Yinshan deposit, one of the large-scale Cu-Pb-Zn-An-Ag polytnetallic deposits, may be named a middle-low temperature subvolcanic hydrothermal deposit and referredto as the "transitional deposit" linking mineralization of the epithermal and porphyry coppertypes. In this paper, the characteristics and structures of ore zoning are briefly described. Onthe basis of the dynamics of ore-forming processes and applying computer numerical simulationtechnique, the mechanism of ore zoning is discussed and a concealed igneous body controllingore deposition at depth of the Yinshan mine is predicted.

Problems and Development Suggestions of Nature Education in Jiangxi Province

The forest coverage rate of Jiangxi Province ranks second in China.It has rich natural resources,a long history of ancient color culture and rich red culture.In the development of nature education,Jiangxi Province has great potential and advantages.This paper introduces the development conditions of nature education in Jiangxi Province,summarizes the problems existing in the development of nature education in Jiangxi Province from the aspects of the types of nature education and the construction of nature education base,such as simple content and single form,imperfect infrastructure and lack of professionals,and puts forward some suggestions on the development of nature education in Jiangxi Province.

Research on Jiangxi’s International Image Based on NOW Corpus

This paper retrieves and classifies reports on Jiangxi from 2010 to June 2024 in the NOW corpus,analyzing the status quo of Jiangxi’s international image portrayed by English news media through word frequency and collocates.It is found that international attention towards Jiangxi is closely related to the holding of the World Conference on VR Industry in Nanchang,and there are apparent regional disparities.With a severe labeling of its mining industry,Jiangxi’s international image lacks independence and distinctiveness,resulting in a relatively monotonous overall image.Based on this,relevant suggestions for further enhancing Jiangxi’s international image are proposed.

An Updated Checklist of the Birds of Jiangxi,China

Complete checklist records are essential to understand regional bird diversity.We update the checklist of the bird species of Jiangxi,China based on numerous reported documents.The updated checklist of the bird species of Jiangxi shows that there are 536 bird species in Jiangxi,which belong to 21 orders,74 families,246 genera.And 48.7% of them are Passeriformes species and 12.3% are Charadriiformes species.Fifty species are classified as threatened.Fourteen of these species are grade I nationally protected wild animals,and 72 species are grade II nationally protected wild animals.In addition,fauna analyses indicate that the Palearctic realm（47.7%） is dominant.As for distribution type,the Oriental type is dominant.Considering the fauna of resident birds,the Oriental realm is dominant.Additionally,the distribution of several species was revised in the checklist.

Risk Evaluation of Monochamus alternatus Hope in Jiangxi Province

[Objective]The study aimed to further strengthen the integrated management of Monochamus alternatus Hope and effectively control its spread and injury in pine forests in Jiangxi Province.[Method] By using the pest risk analysis method,the qualitative and quantitative analysis on risk of M.alternatus in Jiangxi Province was carried out.[Result] The qualitative and quantitative analysis result showed that its risk value R was 1.89,thus confirming that M.alternatus was close to high dangerous forest pest in Jiangxi Province.[Conclusion] The study provided the reference for making the policy decision for control of M.alternatus.

A New Oviraptorid Dinosaur (Theropoda: Oviraptorosauria) from the Late Cretaceous of Jiangxi Province, Southern China

A new oviraptorid dinosaur Jiangxisaurus ganzhouensis gen. et sp. nov., is erected based on a partial skeleton from the Upper Cretaceous Nanxiong Formation of Ganzhou City, Jiangxi Province. The new taxon differs from other oviraptorids in the weakly downturned rostrum of the lower jaw, much-elongated mandible with a height-to-length ratio being about 20% and the length ratio of radius to humerus of about 0.70. This species not only adds a new member to oviraptorid dinosaurs, but also provides more information about oviraptorid paleogeographical distribution in southern China.

Influential Factors of House-purchasing Intention in Work construction Sites among Migrant Workers with a Case of Investigations on 203 Migrant Workers from Jiangxi Province

The research selected 13 factors from individual and family characters, construction site characters and work characters and analyzed the influences on the willingness of purchasing houses on construction sites with Logistic regression mod- el. The results showed that gender, age differences, personality, willingness on fami- ly land conversion, management of enterprises on construction sites, relatives and friends on construction lands, and Job satisfaction were approved by significant testing, but marital status, annual household income, the rate of migrant worker in a household, transportation in work city, and corporate reputation were not approved by significant testing.

猪繁殖与呼吸综合征病毒流行株Jiangxi-3的全基因组序列分析

通过RT-PCR分段扩增PRRSV流行株Jiangxi-3的基因组,参照VR2332序列,根据各片段之间相重叠的区域,将扩增片段的序列依次拼接获得Jiangxi-3完整的全基因组,并通过DNAStar软件对其进行分析。结果表明:Jiangxi-3的Nsp2推导氨基酸发生30个氨基酸的不连续缺失,与HB-1(sh)/2002相比,Nsp2推导的第480位氨基酸由D突变为E,缺失的位置为第481位氨基酸和532～560位氨基酸;Jiangxi-3与2006年Tian Kegong等从江西"高热病"病死猪体内分离的毒株JXA1的各个结构蛋白阅读框的氨基酸同源性为98.0%～100%;Jiangxi-3与HB-1(sh)/2002、VR2332、RespPRRSMLV的Nsp2推导的氨基酸同源性分别为94.7%、77.8%、77.7%,由遗传系统发育树可知与2006年以前分离的毒株相比,Jiangxi-3与HB-1(sh)/2002的亲缘关系较近。说明Jiangxi-3和JXA1极可能由同一毒株HB-1(sh)/2002演化而来。

猪繁殖与呼吸障碍综合征病毒Nsp2基因缺失株Jiangxi-3灭活疫苗免疫效果评价

将猪繁殖与呼吸障碍综合征病毒(PRRSV)Nsp2基因缺失株Jiangxi-3的第9代病毒(Jiangxi-3F9)按常规方法制成油佐剂灭活疫苗,经肌肉注射免疫PRRSV和猪圆环病毒(PCV2)抗原与抗体均为阴性的60日龄健康猪,免疫组分别于初次免疫第21和28天、二次免疫第28天(即初次免疫第28天加强免疫1次)用200LD50的Jiangxi-3 F9进行攻毒,同时各组均设立对照组。通过试验动物体温变化、临床症状、血清PRRS抗体和抗原定期检测结果评价灭活疫苗的免疫效果。结果表明,初次免疫第21和28天免疫组攻毒后体温仍然明显升高,而二次免疫第28天免疫组攻毒后体温升高不明显,最高体温约40℃。初次免疫21-28 d免疫组特异性抗体水平持续升高,初次免疫第21天与第28天抗体水平差异显著(0.01<P<0.05);二次免疫后免疫组抗体水平仍持续升高,第28天可达3.105±0.125,二次免疫第28天与初次免疫28天抗体水平差异显著(0.01<P<0.05)。初次免疫第21天和第28天免疫组攻毒后仍能在血清中检出PRRSV抗原,仍表现不同程度的临床症状,而二免第28天的免疫组攻毒后其PRRSV抗原检出率、发病率、死亡率均为0。表明初次免疫第28天加强免疫一次比免疫一次效果好。

猪繁殖与呼吸障碍综合征病毒Nsp2基因缺失株Jiangxi-3毒力的进一步研究

通过Reed-Muench法检测从江西发生持续高热的病猪体内分离的猪繁殖与呼吸综合征病毒(PRRSV)Nsp2基因缺失株Jiangxi-3第9代(Jiangxi-3F9)的病毒滴度;将此毒株接种于PRRSV和猪圆环病毒2型(PCV2)抗原与抗体均为阴性的60日龄健康猪进行猪半数致死量(LD50)的测定,并且对LD50试验中存活下来的试验猪再次进行较大剂量的攻毒试验,另将病毒接种于PRRSV和PCV2抗原和抗体均为阴性的6月龄健康猪,对所有攻毒试验猪通过体温检测、临床症状观察、RT-PCR、ELISA等方法进一步研究Jiangxi-3F9的毒力。结果表明:Jiangxi-3F9的病毒滴度为105.25TCID50·mL-1,Jiangxi-3F9病毒的LD50为102.·2mL-1。动物试验各项检测结果说明Jiangxi-3F9毒力强。

Revelation on the Drainage Systems of Ancient Villages in Jiangxi Province

Based on rural drainage problems, the research analyzed traditional water culture in ancient vil ages in Jiangxi, as wel as flood control theory, and proposed specific theories and measures for drainage system improvement and construction in order to seek proper rural drainage system and promote rural sustainable develop-ment.

Tapping Advantages and Expanding International and Domestic Networks for Further Integrating Jiangxi with the Rest of the World——Thriving Foreign Related Work in Jiangxi Province

"…enable Jiangxi to become the example of ecological civilization and pacesetter of building beautiful China,and realize the dream of a prosperous,harmonious and beautiful Jiangxi through our earnest efforts."Recent years have witnessed vigorous efforts made by the Provincial Foreign Affairs and Overseas Chinese

Jurassic Intra-plate Basaltic Magmatism in Southeast China:Evidence from Geological and Geochemical Characteristics of the Chebu Gabbroite in Southern Jiangxi Province

Geochemical and isotopic investigations have been carded out on the Chebu gabbroite in southern Jiangxi Province, southeast China and these results are compared with gabbro bodies along the coast of Fujian Province in order to understand their magma sources and tectonic implications. The Chebu intrusion formed at the beginning of the Middle Jurassic （172~4.3 Ma）. These rocks are Ti-rich and Al-poor in major elements, characterized by strong enrichment in large-ion lithophile elements （LILE） and moderate enrichment in high field strength elements （HFSE） and light rare-earth elements CLREE）, without pronounced Nb or Ta anomalies. Age-correlated Sr-Nd isotope ratios show moderately high ranges of （^87Sr/^86Sr）i from 0.7065 to 0.7086 and 0.5124 to 0.5125 of （^143Nd/^144Nd）i. The geochemical characteristics of the Chebu gabbroite suggest that it is notably different from island-arc basalt and similar to intra-plate basaltic rocks. By combining interpretations of its geological and geochemical characteristics and the regional geological development history, the Chebu gabbroitic intrusion is thought to be the product of asthenosphere upwelling and rapid lithosphere extension during a transition of tectonic systems in southeast China. The tectonic environment and source characteristics of the intrusion are different from Cretaceous gabbro bodies along the coast of Fujian Province, The former formed in a tectonic environment of rapid intra-plate lithospheric extension and the source characteristics were of a weakly enriched primitive mantle, whereas the latter originated mainly in a volcanic-magmatic arc extensional tectonic environment and the nature of the source was an enriched mantle with more subduct subducted components.

Geology, Geochemistry and Origin of the Hongshan Porphyry-Cryptoexplosive Breccia Type Copper Deposit in Huichang County, Jiangxi Prvince

The Hongshan porphyry-cryptoexplosive breccia type copper deposit occurs in a metamorphic rock series of the Mesoproterozoic Zhongcun Group. Orebodies are distributed inside and outside porphyry-cryptoexplosive breccia pipes. The deposit involves five ore-forming types, i.e the porphyry type, cryptoexplosive breccia type, contact-zone veinlet-disseminated type, in-pipe fracture-zone filling-replacement type and out-of-pipe fracture-zone filling-replacement type, forming an ore-forming system of “five ore-forming types within a single rock body”. Fluid inclusion and isotope geochemical studies indicate the following: S, Pb, O and Sr were derived from the lower crust, Nd was derived from the continental crust or depleted mantle and rare earth elements (REE) and trace elements have the crustal source characters; fluids consist dominantly of formation water, metamorphic water and ***meteoric water with a part of magmatic mater, heat came from porphyry while the latter originated from partial melting caused by shear heating in the lower crust and upper mantle. According to its origin the deposit is classified as the hypabyssal and near-surface, meso- and hypothermal copper deposit associated with the late Yanshanian porphyry-cryptoexplosive breccia.

Isotopic Chronological Study of the Huangsha-Tieshanlong Quartz Vein-Type Tungsten Deposit and Timescale of Molybdenum Mineralization in Southern Jiangxi Province,China

The Huangsha-Tieshanlong quartz-vein tungsten polymetallic ore deposit, located in the northern Pangushan-Tieshanlong tungsten ore field in eastern Ganxian-Yudu prospecting areas of the Yushan metallogenic belt, is a well-known tungsten deposit in southern Jiangxi province, China. SHRIMP-determined dating of zircons from the Tieshanlong granite yields ages of 168.1±2.1 Ma （n=11, MSWD-1.3）. Rhenium and osmium isotopic dating of molybdenite from the Huangsha quartz-vein tungsten deposit determined by ICP-MS yields a weighted average ages of 153-3 Ma and model ages of 150.22.1 Ma - 155.4-2.3 Ma. The age of the Huangsha tungsten deposit is 10 to 15 Ma later than the Tieshanlong granite, which shows that there might have been another early Late Jurassic magmatic activity between 150 and 160 Ma, a process which is closely related with tungsten mineralization in this area. The Tieshanlong granite, the Hnangsha tungsten deposit and the Pangushan-Tieshanlong ore field were all formed around 150-170 Ma, belonging to products of a Mesozoic second large-scale mineralization. According to the collected molybdenite Re-Os dating results in southern Jiangxi province, the timescale of the associated molybdenum mineralization is 2-6 Ma in the tungsten deposit and the timescale of independent molybdenum mineralization is 1-4 Ma, implying the complexity of tungsten mineralization. Times of molybdenum mineralization are mainly concentrated in the Yanshanian, which includes three stages of 133-135 Ma, 150-162 Ma, and 166-170 Ma, respectively. The 150-162 Ma-stage is in accordance with ages of large-scale WoSn mineralization, which is mainly molybdenum mineralization characterized by associated molybdenum mineralization with development of an even greater-intensity independent molybdenum mineralization. Independent molybdenum mineralization occurred before and after large-scale W-Sn mineralization, which indicates that favorable prospecting period for molybdenum may be in Cretaceous and early late Jurassic.

Precise Dating and Geological Significance of the Caledonian Shangyou Pluton in South Jiangxi Province

The zircon SHRIMP dating age for the Shangyou granites is 464±11 Ma. The geological feature of the pluton is consistent with the isotopic age, which shows that it is a product of Caledonian orogenesis. The Shangyou granites are regarded as peraluminous crust-derived granites to possess the typical geochemical characteristics of calc-alkaline rocks on the active continental margin with enriched Si, K, Al （A/CNK -- 1.11 on average）, HREE, Rb, U, Th and heavily depleted V, Cr, Co, Ni, as well as Ti-Y, Nb-Ta, Zr, Sr, P and Ba, to be commonly corundum normative （av C -- 1.44）. The Shangyou granites with higher 87Sr/86Sr ratios （0.707126-0.712186）, ENd（t） values （-7.29 to -10.22） and （tDM） values （1.52-1.63 Ga）, which are considered to result from partial melting of continental crust metamorphic sedimentary rocks with relatively low of crust maturation degree corresponding to the Middle Proterozoic, to have some possible contributions of mantle-derived components. The Shangyou granites are regarded as post-collision granites, which were formed in a transitional tectonic setting from compression to extension in the Middle Ordovician period after the Yangtze plate was subducted beneath the Cathaysian plate. The Ar-Ar total ages of K-feldspar and biotite are 292.1 Ma and 295.5 Ma respectively, which have recorded information of a late-stage thermal alteration event.