Characteristics of Naturally Formed Nanoparticles in Various Media and Their Prospecting Significance in Chaihulanzi Deposit

In recent years, the exploration of concealed deposits has become extremely urgent as the shortage of surface resources worsens. In this study, naturally formed nanoparticles in five media (deep-seated fault gouge, ascending gas flow, soil, shallow groundwater and deep groundwater) in Chaihulanzi Au deposit, China, were analyzed by transmission electron microscopy. The characteristics of category, shape, lattice parameters, chemical component and association were obtained. The results show that deep media can carry natural nanoparticles to the surface media, resulting in an increased proportion of O and metal chemical valence such as Pb and Cu in nanoparticles. The metal elements Au, Ag, Cu, Zn and As in nanoparticles correspond to those of orebody minerals. Au-Ag-Cu, Fe-As, Cu-Sn and Pb-Zn element associations in nanoparticles are similar to those of mineral composition or orebody paragenesis in Chaihulanzi deposit. Compared with nanoparticle characteristics in deposit and background areas, it can be deduced that natural ore-bearing nanoparticles come from concealed orebodies. With the characteristics of more oxide forms and the dislocation of the crystal lattice, these nanoparticles are formed by faulting and oxidation. Nanoparticles produced in concealed orebodies that migrate from the deep to the surface media could be used for prospecting.

[1]  Yasushi Watanabe,et al.  The metallogenic system deep structure and formation process for the northeastern china compound orogenic belt: Introduction , 2022, Ore Geology Reviews.

[2]  Y. Tong,et al.  Sources of metals and fluids for the Taijiying gold deposit on the northern margin of the North China Craton , 2021, Ore Geology Reviews.

[3]  Jianjin Cao,et al.  Ore-forming elements and their distribution of nanoparticles in the updraft from the Sanshandao concealed deposit, China , 2021 .

[4]  T. Ulrich,et al.  Early Permian lode gold mineralization in the northern North China Craton: Constraints from S-Pb isotope geochemistry and pyrite Re-Os geochronology of the Chaihulanzi deposit , 2021 .

[5]  Jianjin Cao,et al.  Nanoparticles in various media on surfaces of ore deposits: Study of the more than 1000 m deep concealed Shaling gold deposit , 2021, Ore Geology Reviews.

[6]  He Yang,et al.  Geological, fluid inclusion, and O–C–S–Pb–He–Ar isotopic constraints on the genesis of the Honghuagou lode gold deposit, northern North China Craton , 2021, Geochemistry.

[7]  L. Silva,et al.  A review on Pb-bearing nanoparticles, particulate matter and colloids released from mining and smelting activities , 2021, Gondwana Research.

[8]  Xu Li,et al.  Geology, geochronology and tectonic setting of the Chaihulanzi gold deposit in Inner Mongolia, China , 2021, Ore Geology Reviews.

[9]  Jianjin Cao,et al.  Natural uranium-bearing nanoparticles in surface media , 2021, Environmental Chemistry Letters.

[10]  Wanming Zhang,et al.  Preliminary studies on deep-penetrating geochemical methods in exploration for concealed volcanic-type uranium deposit , 2020, IOP Conference Series: Earth and Environmental Science.

[11]  Zixia Lin,et al.  Nanoparticles in groundwater of the Qujia deposit, eastern China: Prospecting significance for deep-seated ore resources , 2020 .

[12]  B. Lafrance,et al.  Gold Remobilization: Insights from Gold Deposits in the Archean Swayze Greenstone Belt, Abitibi Subprovince, Canada , 2020 .

[13]  T. Jiang,et al.  Characterization of metal-bearing particles in groundwater from the Weilasituo Zn-Cu-Ag deposit, Inner Mongolia, China: Implications for mineral exploration , 2020 .

[14]  Jianjin Cao,et al.  TEM analysis of nano- or near-nanoparticles in fault gouge from the Kaxiutata iron deposit (CHN) and the implications for ore body exploration , 2019 .

[15]  S. Flude,et al.  Noble gases confirm plume-related mantle degassing beneath Southern Africa , 2019, Nature Communications.

[16]  Ting Liu,et al.  Extraction of soils above concealed lithium deposits for rare metal exploration in Jiajika area: A pilot study , 2019, Applied Geochemistry.

[17]  Jianjin Cao,et al.  Metal-containing nanoparticles derived from concealed metal deposits: An important source of toxic nanoparticles in aquatic environments. , 2019, Chemosphere.

[18]  Yingkui Li,et al.  A study of metal-bearing nanoparticles from the Kangjiawan Pb-Zn deposit and their prospecting significance , 2019, Ore Geology Reviews.

[19]  Zhenghai Wang,et al.  A TEM study of particles carried by ascending gas flows from the Bairendaba lead-zinc deposit, Inner Mongolia, China , 2019, Ore Geology Reviews.

[20]  Q. Wan,et al.  Sorption of Differently Charged Gold Nanoparticles on Synthetic Pyrite , 2018, Minerals.

[21]  T. Jiang,et al.  Discovery and prospecting significance of metal-bearing nanoparticles within natural invertebrate tissues , 2018, Ore Geology Reviews.

[22]  Jianjin Cao,et al.  Discovery of nano-sized gold particles in natural plant tissues , 2018, Environmental Chemistry Letters.

[23]  A. Stohl,et al.  Lead pollution recorded in Greenland ice indicates European emissions tracked plagues, wars, and imperial expansion during antiquity , 2018, Proceedings of the National Academy of Sciences.

[24]  Yingkui Li,et al.  TEM observations of particles in groundwater and their prospecting significance in the Bofang copper deposit, Hunan, China , 2018 .

[25]  Zhenghai Wang,et al.  Transmission Electron Microscopy Analysis on Fault Gouges from the Depths of the Bairendaba Polymetallic Deposit, Inner Mongolia, China , 2017 .

[26]  R. Haszeldine,et al.  The physical characteristics of a CO2 seeping fault: the implications of fracture permeability for carbon capture and storage integrity , 2017 .

[27]  Hao-Long Zhou,et al.  Nano- to micron-scale particulate gold hosted by magnetite: A product of gold scavenging by bismuth melts , 2017 .

[28]  T. Jiang,et al.  Prospecting Application of Nanoparticles and Nearly Nanoscale Particles Within Plant Tissues , 2017 .

[29]  Mohammed Ali Berawi,et al.  Advanced nanomaterials in oil and gas industry: Design, application and challenges , 2017 .

[30]  Mingyue Hu,et al.  Identification of metal sources in Geogas from the Wangjiazhuang copper deposit, Shandong, China: Evidence from lead isotopes , 2017 .

[31]  Jianjin Cao,et al.  Characteristics of soil particles in the Xiaohulishan deposit, Inner Mongolia, China , 2016 .

[32]  Qingfei Wang,et al.  Gold mineralization in China: Metallogenic provinces, deposit types and tectonic framework , 2016 .

[33]  P. Hopke,et al.  The discovery of the metallic particles of groundwater from the Dongshengmiao polymetallic deposit, Inner Mongolia, and their prospecting significance , 2016 .

[34]  Jianjin Cao,et al.  TEM observations of particles based on sampling in gas and soil at the Dongshengmiao polymetallic pyrite deposit, Inner Mongolia, Northern China , 2015 .

[35]  Jianjin Cao,et al.  TEM study on particles transported by ascending gas flow in the Kaxiutata iron deposit, Inner Mongolia, North China , 2015 .

[36]  P. Hopke,et al.  Study of Carbon‐Bearing Particles in Ascending Geogas Flows in the Dongshengmiao Polymetallic Pyrite Deposit, Inner Mongolia, China , 2015 .

[37]  Yansheng Zhang,et al.  Methane-rich Fluid of Chaihulanzi Gold Deposit , 2014 .

[38]  M. Schindler,et al.  High-resolution lake sediment reconstruction of industrial impact in a world-class mining and smelting center, Sudbury, Ontario, Canada , 2013 .

[39]  YunAn Hu,et al.  Geoelectrochemical-Extraction Measurement Method to Look for Hidden Lead-Zinc Ore Deposit and Prospecting Effect , 2013 .

[40]  P. Hopke,et al.  TEM study of geogas-transported nanoparticles from the Fankou lead–zinc deposit, Guangdong Province, South China , 2013 .

[41]  J. Erzinger,et al.  Geogas transport in fractured hard rock - Correlations with mining seismicity at 3.54 km depth, TauTona gold mine, South Africa , 2011 .

[42]  R. Hough,et al.  Trace metal nanoparticles in pyrite , 2011 .

[43]  Jianjin Cao Migration mechanisms of gold nanoparticles explored in geogas of the Hetai ore district, southern China , 2011 .

[44]  Jianjin Cao,et al.  Particles carried by ascending gas flow at the Tongchanghe copper mine, Guizhou Province, China , 2010 .

[45]  H. W. Li,et al.  Simulation of adsorption of gold nanoparticles carried by gas ascending from the Earth's interior in alluvial cover of the middle-lower reaches of the Yangtze River. , 2010 .

[46]  R. Hu,et al.  TEM observation of geogas-carried particles from the Changkeng concealed gold deposit, Guangdong Province, South China , 2009 .

[47]  Nanshi Zeng,et al.  CHIM-geoelectrochemical method in search of concealed mineralisation in China and Australia , 2008 .

[48]  R. Noble,et al.  Naturally occurring gold nanoparticles and nanoplates , 2008 .

[49]  F. Bierlein,et al.  Bimodal Distribution of Gold in Pyrite and Arsenopyrite: Examples from the Archean Boorara and Bardoc Shear Systems, Yilgarn Craton, Western Australia , 2008 .

[50]  Qingdong Zeng,et al.  Integrated geological and geophysical exploration for concealed ores beneath cover in the Chaihulanzi goldfield, northern China , 2006 .

[51]  Liu Daxin The Mafic Granulite Xenoliths and Its Implications to Mineralization in Chaihulanzi Gold Deposit, Inner Mongolian, China , 2006 .

[52]  R. Hu,et al.  Simulation test on migration of geogas-carrying gold nanoparticles in slope sediments , 2005 .

[53]  R. Ewing,et al.  “Invisible„ gold revealed: Direct imaging of gold nanoparticles in a Carlin-type deposit , 2004 .

[54]  S. Wilde,et al.  A review of the geodynamic setting of large-scale Late Mesozoic gold mineralization in the North China Craton: an association with lithospheric thinning , 2003 .

[55]  S. Lombardi,et al.  Short- and long-term gas hazard: the release of toxic gases in the Alban Hills volcanic area (central Italy) , 2003 .

[56]  Mark C. Barnes,et al.  Generation of charged clusters during thermal evaporation of gold , 2002 .

[57]  Nils-Axel Mörner,et al.  Carbon degassing from the lithosphere , 2002 .

[58]  T. Williams,et al.  Application of enzyme leach soil analysis for epithermal gold exploration in the Andes of Ecuador , 2002 .

[59]  G. Etiope,et al.  Migration of carrier and trace gases in the geosphere: an overview , 2002 .

[60]  M. Gloor,et al.  Geochemistry of the peat bog at Etang de la Gruère, Jura Mountains, Switzerland, and its record of atmospheric Pb and lithogenic trace metals (Sc, Ti, Y, Zr, and REE) since 12,370 14 C yr BP , 2001 .

[61]  J. Cline Timing of Gold and Arsenic Sulfide Mineral Deposition at the Getchell Carlin-Type Gold Deposit, North-Central Nevada , 2001 .

[62]  She Hong TECTONIC AND MAGMATIC ACTIVITIES IN EARLY MESOZOIC AND THEIR CONTROLLING ON GOLD MINERALIZATION IN HONGHUAGOU GOLD ORE FIELD, INNER MONGOLIA , 2000 .

[63]  H. Waldron,et al.  Biogeochemistry of the Ballarat East goldfield, Victoria, Australia , 1999 .

[64]  L. Malmqvist,et al.  Geogas prospecting – an ideal industrial application of PIXE , 1999 .

[65]  J. Toutain,et al.  Gas geochemistry and seismotectonics: a review , 1999 .

[66]  Ong Chunhan,et al.  Experimental observation of the nano-scale particles in geogas matters and its geological significance , 1998 .

[67]  A. Mann,et al.  Application of the mobile metal ion technique to routine geochemical exploration , 1998 .

[68]  P. Prince,et al.  The Evaluation of Geological Exploration Samples using Multi- element Mobile Metal Ion (MMI-M) Selective Weak Extraction and Inductively Coupled Plasma Mass Spectrometry (ICP-MS) , 1998 .

[69]  I. S. Goldberg,et al.  New methods of regional exploration for blind mineralization: Application in the USSR , 1992 .

[70]  A. Meier,et al.  Enzyme leaching of surficial geochemical samples for detecting hydromorphic trace-element anomalies associated with precious-metal mineralized bedrock buried beneath glacial overburden in northern Minnesota , 1990 .

[71]  L. Malmqvist,et al.  Geogas prospecting: a new tool in the search for concealed mineralizations , 1990 .

[72]  L. Malmqvist,et al.  Trace elements in the geogas and their relation to bedrock composition , 1987 .

[73]  L. Malmqvist,et al.  Experimental evidence for an ascending microflow of geogas in the ground , 1984 .

[74]  Lennart Malmqvist,et al.  Evidence for nondiffusive transport of 86Rn in the ground and a new physical model for the transport , 1982 .

[75]  T. Gold,et al.  The deep earth gas hypothesis , 1980 .