Genetic Relationship between Granite and Fluorite Mineralization in the Shuanghuajiang Fluorite Deposit, Northern Guangxi, South China: Evidence from Geochronology, REE, and Fluid Geochemistry

Hydrothermal vein-type fluorite deposits are the most important metallogenic type of fluorite deposits in South China, most of which are closely related to granitoid in space; however, the genetic relationship between granitoid and fluorite mineralization remains controversial. The Shuanghuajiang fluorite deposit in northern Guangxi of South China is a typical vein-type fluorite deposit hosted in a granite pluton, with the orebodies occurring within brittle faults. Zircon U-Pb dating of the hosting Xiangcaoping granite yields an emplacement age of 228.04 ± 0.76 Ma (MSWD = 0.072). Fluorite Sm-Nd dating yields an isochron age of 185 ± 18 Ma. The new age data indicate that the fluorite deposit was precipitated significantly later than the emplacement of the hosting Xiangcaoping granite pluton. The fluorite and granite exhibit similar rare earth element (REE) patterns with negative Eu anomalies, suggesting that fluorine (F) was derived from the granite. The fluorite fluid inclusions show a homogeneous temperature mainly ranging between 165 °C and 180 °C. Salinity is typically less than 1% NaCl eqv, while the δ18OV-SMOW and δDV-SMOW values are between −5.2‰–−6.1‰ and −17.35‰–−23.9‰, respectively. These indicate that the ore-forming fluids were a NaCl-H2O system with medium-low temperature and low salinity, which is typical for meteoric water. Given the combined evidence of geochronology, REE, and fluid geochemistry, the mineralization of the Shuanghuajiang fluorite deposit is unrelated to magmatic-hydrothermal activity but achieved via hydrothermal circulation and leaching mechanisms. Our study presents a genetic relationship between the fluorite deposit and granitoids based on an example of northern Guangxi, providing a better understanding of the genesis of hydrothermal vein-type fluorite deposits in granitoids outcropping areas.

[1]  Q. Zheng,et al.  Resolving the Tectonic Setting of South China in the Late Paleozoic , 2022, Geophysical Research Letters.

[2]  T. Algeo,et al.  A general ore formation model for metasediment-hosted Sb-(Au-W) mineralization of the Woxi and Banxi deposits in South China , 2022, Chemical Geology.

[3]  Huimin Su,et al.  Textural features and in situ trace element analysis of fluorite from the Wujianfang fluorite deposit, Inner Mongolia (NE China): Insights into fluid metasomatism and ore-forming process , 2022, Ore Geology Reviews.

[4]  Jinhua Cheng,et al.  Production quota policy in China: Implications for sustainable supply capacity of critical minerals , 2021 .

[5]  Richard C. Bayless,et al.  In situ LA ICP-MS analysis of trace elements in scheelite from the Xuefeng Uplift Belt, South China and its metallogenic implications , 2021, Ore Geology Reviews.

[6]  Qian-hong Wu,et al.  Fluid inclusion, H–O–S isotope and rare earth element constraints on the mineralization of the Dong’an Sb deposit, South China , 2020 .

[7]  Katarzyna Guzik,et al.  Approach to identification and classification of the key, strategic and critical minerals important for the mineral security of Poland , 2020 .

[8]  Chaoqun Yao,et al.  Fluorite deposits in China: Geological features, metallogenic regularity, and research progress , 2020 .

[9]  Xiaofeng Li,et al.  Multistage magmatic-hydrothermal activity and W-Cu mineralization at Jiepai, Guangxi Zhuang Autonomous Region, South China: Constraints from geochronology and Nd-Sr-Hf-O isotopes , 2020 .

[10]  L. Bagas,et al.  Fluorite deposits in the Zhejiang Province, southeast China: The possible role of extension during the late stages in the subduction of the Paleo-Pacific oceanic plate, as indicated by the Gudongkeng fluorite deposit , 2020 .

[11]  Long Ren,et al.  Ages and genesis of W-Sn and Ta-Nb-Sn-W mineralization associated with the Limu granite complex, Guangxi, China , 2020 .

[12]  Wei Lin,et al.  Cretaceous Episodic Extension in the South China Block, East Asia: Evidence From the Yuechengling Massif of Central South China , 2019, Tectonics.

[13]  Xiaofeng Li,et al.  Multiple-stage tungsten mineralization in the Silurian Jiepai W skarn deposit, South China: Insights from cathodoluminescence images, trace elements, and fluid inclusions of scheelite , 2019, Journal of Asian Earth Sciences.

[14]  Zhang Yi-xi,et al.  The brittle-ductile shearing and uranium metallogenesis of the Motinaling dome in the southwestern Jiangnan Orogenic Belt , 2019, Acta Petrologica Sinica.

[15]  Changqian Ma,et al.  A source-depleted Early Jurassic granitic pluton from South China: Implication to the Mesozoic juvenile accretion of the South China crust , 2018 .

[16]  Chen Libo,et al.  Geochemical evidence of the source of ore-forming materials from Dazhuyuan fluorite deposit in northeastern Guizhou , 2018 .

[17]  Alexis Van Maercke,et al.  EU Methodology for Critical Raw Materials Assessment: Policy Needs and Proposed Solutions for Incremental Improvements , 2017 .

[18]  T. Ntaflos,et al.  Mineralogical, geochemical and Sr-Nd isotopes characteristics of fluorite-bearing granites in the Northern Arabian-Nubian Shield, Egypt: Constraints on petrogenesis and evolution of their associated rare metal mineralization , 2017 .

[19]  Shou‐ting Zhang,et al.  Geochronology, geochemistry, fluid inclusion and C, O and Hf isotope compositions of the Shuitou fluorite deposit, Inner Mongolia, China , 2017 .

[20]  X. Qiu,et al.  Geochemistry and Hf–Nd isotope characteristics and forming processes of the Yuntoujie granites associated with W–Mo deposit, Guangxi, South China , 2017 .

[21]  Di Zhang,et al.  A study on the Dushiling tungsten-copper deposit in the Miao’ershan-Yuechengling area, Northern Guangxi, China: Implications for variations in the mineralization of multi-aged composite granite plutons , 2016, Science China Earth Sciences.

[22]  Jinxiang Wang,et al.  Unusually low TEX86 values in the transitional zone between Pearl River estuary and coastal South China Sea: Impact of changing archaeal community composition , 2015 .

[23]  N. Rubinstein,et al.  Origin and age of rift related fluorite and manganese deposits from the San Rafael Massif, Argentina , 2015 .

[24]  Wang Ji-pin,et al.  Metallogenic regularities of fluorite deposits in China , 2015 .

[25]  D. Zhang Quartz-vein Type Tungsten Mineralization Associated with the Indosinian (Triassic) Gaoling Granite,Miao'ershan Area,Northern Guangxi , 2015 .

[26]  U. Schwarz-Schampera,et al.  Mineralogy of high-field-strength elements (Y, Nb, REE) in the world-class Vergenoeg fluorite deposit, South Africa , 2015 .

[27]  Wang Ji-pin The classification of fluorite deposits in China , 2014 .

[28]  Zhang Shoutin Characteristics of ore-forming fluids and mineralization processes of the Shuitou fluorite deposit in Linxi,Inner Mongolia Autonomous Region , 2014 .

[29]  Rucheng Wang,et al.  Timing of hydrothermal activity associated with the Douzhashan uranium-bearing granite and its significance for uranium mineralization in northeastern Guangxi, China , 2013 .

[30]  N. M. Mahdy,et al.  Trace and REE element geochemistry of fluorite and its relation to uranium mineralizations, Gabal Gattar Area, Northern Eastern Desert, Egypt , 2013, Arabian Journal of Geosciences.

[31]  Yang Zhen Geochronology and Geochemical Characteristics of Metallogenetic Pluton in the Youmaling Tungsten Mining Area,Northern Guangxi Province,and Its Geological Significance , 2013 .

[32]  Xia Xuehui,et al.  Hydrothermal Sedimentary Mineralization of the Super‐large Bamianshan Fluorite Deposit in Zhejiang Province, China , 2012 .

[33]  Wei-dong Sun,et al.  Indosinian isotope ages of plutons and deposits in southwestern Miaoershan-Yuechengling, northeastern Guangxi and implications on Indosinian mineralization in South China , 2012 .

[34]  L. Xiaofeng Spatial and Temporal Distributions and the Geological Setting of the W-Sn-Mo-Nb-Ta Deposits at the Northeast Guangxi, Southe China , 2012 .

[35]  Liang Zhong-peng Sedimentary Genesis Feature of Bamianshan Unusual Large Fluorite Deposit in Zhejiang Province , 2010 .

[36]  M. Pownceby,et al.  Oxidation state of europium in scheelite: Tracking fluid–rock interaction in gold deposits , 2008 .

[37]  Jiang Shao,et al.  Geochemical characteristics and geochronology of the Douzhashan granite,northeastern Guangxi Province,China. , 2008 .

[38]  G. Levresse,et al.  The “El Pilote” fluorite skarn: A crucial deposit in the understanding and interpretation of the origin and mobilization of F from northern Mexico deposits , 2006 .

[39]  G. Markl,et al.  REE systematics in hydrothermal fluorite , 2005 .

[40]  P. Burnard,et al.  Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer , 2003 .

[41]  J. Pironon,et al.  Fluorite deposits at Encantada–Buenavista, Mexico: products of Mississippi Valley type processes , 2003 .

[42]  R. Romer,et al.  Tracing element sources of hydrothermal mineral deposits: REE and Y distribution and Sr-Nd-Pb isotopes in fluorite from MVT deposits in the Pennine Orefield, England , 2003 .

[43]  W. Griffin,et al.  Igneous zircon: trace element composition as an indicator of source rock type , 2002 .

[44]  D. Günther,et al.  Determination of Forty Two Major and Trace Elements in USGS and NIST SRM Glasses by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry , 2002 .

[45]  Hnigs Loudi THE CHARACTERISTICS AND ITS FIXED POSITION MECHANISM OF GRANITE UNIT AND SUPER-UNIT OF MIAOER MOUNTAIN , 2002 .

[46]  L. P. Black,et al.  Metamorphic zircon formation by solid‐state recrystallization of protolith igneous zircon , 2000 .

[47]  D. Borrok,et al.  The Vergenoeg magnetite-fluorite deposit, South Africa; support for a hydrothermal model for massive iron oxide deposits , 1998 .

[48]  M. Bau Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium , 1991 .

[49]  S. Wood The aqueous geochemistry of the rare-earth elements and yttrium: 2. Theoretical predictions of speciation in hydrothermal solutions to 350°C at saturation water vapor pressure , 1990 .

[50]  S. Wood The aqueous geochemistry of the rare-earth elements and yttrium: 2. Theoretical predictions of speciation in hydrothermal solutions to 350°C at saturation water vapor pressure , 1990 .

[51]  C. Anglin,et al.  Sm-Nd and Rb-Sr isotope systematics of scheelites: Possible implications for the age and genesis of vein-hosted gold deposits , 1989 .

[52]  R. Rye,et al.  The chemical and thermal evolution of the fluids in the Cave-in-Rock fluorspar district, Illinois; stable isotope systematics at the Deardorff Mine , 1988 .

[53]  R. Bodnar,et al.  Freezing point depression of NaCl-KCl-H 2 O solutions , 1988 .

[54]  S. Sheppard Characterization and isotopic variations in natural waters , 1986 .

[55]  E. Deloule The genesis of fluorspar hydrothermal deposits at Montroc and Le Burc, the Tarn, as deduced from fluid inclusion analysis , 1982 .

[56]  P. Parekh,et al.  The application of Tb/Ca-Tb/La abundance ratios to problems of fluorspar genesis , 1976 .

[57]  H. Taylor The Application of Oxygen and Hydrogen Isotope Studies to Problems of Hydrothermal Alteration and Ore Deposition , 1974 .

[58]  H. Ohmoto,et al.  Hydrogen and Oxygen Isotopic Compositions of Fluid Inclusions in the Kuroko Deposits, Japan , 1974 .

[59]  R. Clayton,et al.  The use of bromine pentafluoride in the extraction of oxygen from oxides and silicates for isotopic analysis , 1963 .

[60]  M. Santosh,et al.  Fault-controlled carbonate-hosted barite-fluorite mineral systems: The Shuanghe deposit, Yangtze Block, South China , 2022 .