Quadratic investigation of geochemical distribution by backward elimination approach at Glojeh epithermal Au(Ag)-polymetallic mineralization, NW Iran

Darabi-Golestan Farshad , Hezarkhani Ardeshir

Journal of Central South University ›› 2018, Vol. 25 ›› Issue (2) : 342 -356.

PDF
Journal of Central South University ›› 2018, Vol. 25 ›› Issue (2) : 342 -356. DOI: 10.1007/s11771-018-3741-8
Article

Quadratic investigation of geochemical distribution by backward elimination approach at Glojeh epithermal Au(Ag)-polymetallic mineralization, NW Iran

Author information +
History +
PDF

Abstract

The correspondence analysis will describe elemental association accompanying an indicator samples. This analysis indicates strong mineralization of Ag, As, Pb, Te, Mo, Au, Zn and to a lesser extent S, W, Cu at Glojeh polymetallic mineralization, NW Iran. This work proposes a backward elimination approach (BEA) that quantitatively predicts the Au concentration from main effects (X), quadratic terms (X2) and the first order interaction (Xi×Xj) of Ag, Cu, Pb, and Zn by initialization, order reduction and validation of model. BEA is done based on the quadratic model (QM), and it was eliminated to reduced quadratic model (RQM) by removing insignificant predictors. During the QM optimization process, overall convergence trend of R2, R2(adj) and R2(pred) is obvious, corresponding to increase in the R2(pred) and decrease of R2. The RQM consisted of (threshold value, Cu, Ag×Cu, Pb×Zn, and Ag2–Pb2) and (Pb, Ag×Cu, Ag×Pb, Cu×Zn, Pb×Zn, and Ag2) as main predictors of optimized model according to 288 and 679 litho-samples in trenches and boreholes, respectively. Due to the strong genetic effects with Au mineralization, Pb, Ag2, and Ag×Pb are important predictors in boreholes RQM, while the threshold value is known as an important predictor in the trenches model. The RQMs R2(pred) equal 74.90% and 60.62% which are verified by R2 equal to 73.9% and 60.9% in the trenches and boreholes validation group, respectively.

Keywords

correspondence analysis / first order interaction / reduced quadratic model (RQM) / optimized model / order reduction and validation / strong genetic effects

Cite this article

Download citation ▾
Darabi-Golestan Farshad, Hezarkhani Ardeshir. Quadratic investigation of geochemical distribution by backward elimination approach at Glojeh epithermal Au(Ag)-polymetallic mineralization, NW Iran. Journal of Central South University, 2018, 25(2): 342-356 DOI:10.1007/s11771-018-3741-8

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

BorradaileG JStatistics of earth science data: Their distribution in time, space and orientation [M], 2013, Berlin, Springer Science & Business Media

[2]

GrahamM W, MillerD J. Unsupervised learning of parsimonious mixtures on large spaces with integrated feature and component selection [J]. IEEE Transactions on Signal Processing, 2006, 54: 1289-1303

[3]

SenZSpatial modeling principles in earth sciences [M], 2009, Berlin, Springer Science & Business Media

[4]

Abdul-WahabS A, BakheitC S, Al-AlawiS M. Principal component and multiple regression analysis in modelling of ground-level ozone and factors affecting its concentrations [J]. Environmental Modelling & Software., 2005, 20: 1263-1271

[5]

HessamiM, GachonP, OuardaT B, St-HilaireA. Automated regression-based statistical downscaling tool [J]. Environmental Modelling & Software, 2008, 23: 813-834

[6]

LiS, ZhaoZ, MiaomiaoX, WangY. Investigating spatial non-stationary and scale-dependent relationships between urban surface temperature and environmental factors using geographically weighted regression [J]. Environmental Modelling & Software, 2010, 25: 1789-1800

[7]

MillerD J, BrowningJ. A mixture model and EM-based algorithm for class discovery, robust classification, and outlier rejection in mixed labeled/unlabeled data sets [J]. IEEE Transactions on Pattern Analysis and Machine Intelligence, 2003, 25: 1468-1483

[8]

ChunY, GriffithD A, LeeM, SinhaP. Eigenvector selection with stepwise regression techniques to construct eigenvector spatial filters [J]. Journal of Geographical Systems, 2016, 18: 67-85

[9]

CordellH J, ClaytonD G. A unified stepwise regression procedure for evaluating the relative effects of polymorphisms within a gene using case/control or family data: Application to HLA in type 1 diabetes [J]. The American Journal of Human Genetics, 2002, 70: 124-141

[10]

GranianH, TabatabaeiS H, AsadiH H, CarranzaE J M. Multivariate regression analysis of lithogeochemical data to model subsurface mineralization: A case study from the Sari Gunay epithermal gold deposit, NW Iran [J]. Journal of Geochemical Exploration, 2015, 148: 249-258

[11]

PasandidehS H R, NiakiS T A, FarM H. Optimization of vendor managed inventory of multiproduct EPQ model with multiple constraints using genetic algorithm [J]. The International Journal of Advanced Manufacturing Technology, 2014, 71: 365-376

[12]

AzadiT E, AlmasganjF. Using backward elimination with a new model order reduction algorithm to select best double mixture model for document clustering [J]. Expert Systems with Applications, 2009, 36: 10485-10493

[13]

FigueiredoM A T, JainA K. Unsupervised learning of finite mixture models [J]. IEEE Transactions on Pattern Analysis and Machine Intelligence, 2002, 24: 381-396

[14]

MyersR H, MontgomeryD C, Anderson-CookC MResponse surface methodology: Process and product optimization using designed experiments [M], 2016, Hoboken, NJ, John Wiley & Sons

[15]

MohammadiR, MohammadifarM A, MortazavianA M, RouhiM, GhasemiJ B, DelshadianZ. Extraction optimization of pepsin-soluble collagen from eggshell membrane by response surface methodology (RSM) [J]. Food Chemistry, 2016, 190: 186-193

[16]

SamalA R, MohantyM K, FifarekR H. Backward elimination procedure for a predictive model of gold concentration [J]. Journal of Geochemical Exploration, 2008, 97: 69-82

[17]

FahrmeirL, KneibT, LangS, MarxBRegression: Models, methods and applications [M], 2013, Berlin, Springer Science & Business Media

[18]

GranianH, TabatabaeiS H, AsadiH H, CarranzaE J M. Application of discriminant analysis and support vector machine in mapping gold potential areas for further drilling in the Sari-Gunay Gold Deposit, NW Iran [J]. Natural Resources Research, 2016, 25: 145-159

[19]

YadavV, MuellerK L, MichalakA M. A backward elimination discrete optimization algorithm for model selection in spatio-temporal regression models [J]. Environmental Modelling & Software, 2013, 42: 88-98

[20]

EvrendilekG A, AvsarY K, EvrendilekF. Modelling stochastic variability and uncertainty in aroma active compounds of PEF-treated peach nectar as a function of physical and sensory properties, and treatment time [J]. Food Chemistry, 2016, 190: 634-642

[21]

PardoeIApplied regression modeling: A business approach [M], 2012, Hoboken, NJ, John Wiley & Sons

[22]

MehrabiB, SianiM G, AziziH. The genesis of the epithermal gold mineralization at North Glojeh veins, NW Iran [J]. IJSAR, 2014, 15: 479-497

[23]

ChinnasamyS S, UkenR, ReinhardtJ, SelbyD, JohnsonS. Pressure, temperature, and timing of mineralization of the sedimentary rock-hosted orogenic gold deposit at Klipwal, southeastern Kaapvaal Craton, South Africa [J]. Mineralium Deposita, 2015, 50: 739-766

[24]

GranceaL, BaillyL, LeroyJ, BanksD, MarcouxE, MilesiJ, CuneyM, AndreA, IstvanD, FabreC. Fluid evolution in the Baia Mare epithermal gold/polymetallic district, Inner Carpathians, Romania [J]. Mineralium Deposita, 2002, 37: 630-647

[25]

Martinz-AbadI, CepedalA, AriasD, FuertesfuenteM. The Au–As (Ag–Pb–Zn–Cu–Sb) veindisseminated deposit of Arcos (Lugo, NW Spain): Mineral paragenesis, hydrothermal alteration and implications in invisible gold deposition [J]. Journal of Geochemical Exploration, 2015, 151: 1-16

[26]

AbdiH, WilliamsL J, ValentinD. Multiple factor analysis: Principal component analysis for multi-table and multi-block data sets [J]. Computational Statistics, 2013, 5: 149-179

[27]

GolestanF D, HezarkhaniA, ZareM. Interpretation of the sources of radioactive elements and relationship between them by using multivariate analyses in anzali wetland area [J]. Geoinformatics & Geostatistics: An Overview, 2013, 1(4): 1-10

[28]

RoshaniP, MokhtariA R, TabatabaieS H. Objective based geochemical anomaly detection— application of discriminant function analysis in anomaly delineation in the Kuh Panj porphyry Cu mineralization (Iran) [J]. Journal of Geochemical Exploration, 2013, 130: 65-73

[29]

DidayE, Noirhomme-FraitureMSymbolic data analysis and the SODAS software [M], 2008, Hoboken, NJ, Wiley Online Library

[30]

GlennieKW. Cretaceous tectonic evolution of Arabia's eastern plate margin: a tale of two oceans [M]//Middle East models of Jurassic/Cretaceous carbonate systems. SEPM (Society for Sedimentary Geology), Spec. Publ., 2000, 69: 9-20

[31]

MohajjelM, FergussonC. Jurassic to Cenozoic tectonics of the Zagros Orogen in northwestern Iran [J]. International Geology Review, 2014, 56: 263-287

[32]

RichardsJ P. Tectonic, magmatic, and metallogenic evolution of the Tethyan orogen: From subduction to collision [J]. Ore Geology Reviews, 2015, 70: 323-345

[33]

VerdelC, WernickeB P, HassanzadehJ, GuestB. A Paleogene extensional arc flare-up in Iran [J]. Tectonics, 201130

[34]

YangZ, HouZ, WhiteN C, ChangZ, LiZ, SongY. Geology of the post-collisional porphyry copper–molybdenum deposit at Qulong, Tibet [J]. Ore Geology Reviews, 2009, 36: 133-159

[35]

AgardP, OmraniJ, JolivetL, MouthereauF. Convergence history across Zagros (Iran): Constraints from collisional and earlier deformation [J]. International Journal of Earth Sciences, 2005, 94: 401-419

[36]

AziziH, AsaharaY, MehrabiB, ChungS L. Geochronological and geochemical constraints on the petrogenesis of high-K granite from the Suffi abad area, Sanandaj-Sirjan Zone, NW Iran [J]. Chemie der Erde-Geochemistry, 2011, 71: 363-376

[37]

AlianiF, MaanijouM, SabouriZ, SepahiA A. Petrology, geochemistry and geotectonic environment of the Alvand Intrusive Complex, Hamedan, Iran [J]. Chemie der Erde-Geochemistry, 2012, 72: 363-383

[38]

GolonkaJ. Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic [J]. Tectonophysics, 2004, 381: 235-373

[39]

SarkarinejadK. The role of the zagros suture on three dimensional deformation pattern in eghlid-deh bid area of Iran [J]. Journal of Sciences, Islamic Republic of Iran, 2010, 21(2): 155-167

[40]

GhasemiA, TalbotC. A new tectonic scenario for the Sanandaj–Sirjan Zone (Iran) [J]. Journal of Asian Earth Sciences, 2006, 26: 683-693

[41]

Darabi-GolestanF, Ghavami-RiabiR, KhalokakaieR, Asadi-HaroniH, Seyedrahimi-NyaraghM. Interpretation of lithogeochemical and geophysical data to identify the buried mineralized area in Cu-Au porphyry of Dalli-Northern Hill [J]. Arabian Journal of Geosciences, 2013, 6: 4499-4509

[42]

Eftekhar-NezhadJ N M, ValehN. Geology of Tarom-Talesh area [R]. Geological Survey of Iran. Note No.16 with Map 1:100 u, 1965129

[43]

MehrabiB, SianiM G, GoldfarbR, AziziH, GanerodM, MarshE E. Mineral assemblages, fluid evolution, and genesis of polymetallic epithermal veins, Glojeh district, NW Iran [J]. Ore Geology Reviews, 2016, 78: 41-57

[44]

NabaviM. An introduction to the geology of Iran [R]. Geological survey of Iran, 1976110

[45]

GhorbaniMThe economic geology of Iran: mineral deposits and natural resources [M], 2013, Berlin, Springer Science & Business Media

[46]

BahajroyM, TakiS. Study of the mineralization potential of the intrusives around Valis (Tarom-Iran) [J]. Earth Sciences Research Journal, 2014, 18: 123-129

[47]

GhorbaniM. Alborz zone or Alborz geology state and its mineralization potential. [C]//1st Conference of Alborz and Caspian Sea Marginal Regions Earth Sciences, Tehran, Iran, 2005

[48]

Fuertes-FuenteM, CepedalA, LimaA, DoriaA, dos Anjos RibeiroM, GuedesA. The Au-bearing vein system of the Limarinho deposit (northern Portugal): Genetic constraints from Bi-chalcogenides and Bi–Pb–Ag sulfosalts, fluid inclusions and stable isotopes [J]. Ore Geology Reviews, 2016, 72: 213-231

[49]

GrosM, LorandJ P, LuguetA. Analysis of platinum group elements and gold in geological materials using NiS fire assay and Te coprecipitation; the NiS dissolution step revisited [J]. Chemical Geology, 2002, 185: 179-190

[50]

JuvonenR, KontasE. Comparison of three analytical methods in the determination of gold in six Finnish gold ores, including a study on sample preparation and sampling [J]. Journal of Geochemical Exploration, 1999, 65: 219-229

[51]

KrishnaH, KumarK. Reliability estimation in Lindley distribution with progressively type II right censored sample [J]. Mathematics and Computers in Simulation, 2011, 82: 281-294

[52]

PatinhaC, CorreiaE, da SilvaE F, SimoesA, ReisP, MorgadoF, FonsecaE C. Definition of geochemical patterns on the soil of Paul de Arzila using correspondence analysis [J]. Journal of Geochemical Exploration, 2008, 98: 34-42

[53]

Darabi-GolestanF, HezarkhaniA, ZareM. Assessment of 226Ra, 238U, 232Th, 137Cs and 40K activities from the northern coastline of Oman Sea (water and sediments) [J]. Marine Pollution Bulletin, 2017, 118(1): 197-205

[54]

Darabi-GolestanF, Ghavami RiabiR, MajlesiMJ, MemarzadeM, Asadi HarooniH. Identify and separation of anomall variable using correspondence and discriminant analyses methods at Northern–Dalli area [J]. analytical and Numerical Method in Minning Engineering, 2012, 3: 35-45

[55]

Darabi-GolestanF, HezarkhaniA. Evaluation of elemental mineralization rank using fractal and multivariate techniques and improving the performance by log-ratio transformation [J]. Journal of Geochemical Exploration, 2017

[56]

MohamadiN M, HezarkkhaniA, SaljooghiB S. Separation of a geochemical anomaly from background by fractal and U-statistic methods, a case study: Khooni district, Central Iran [J]. Chemie der Erde-Geochemistry, 2016, 76: 491-499

AI Summary AI Mindmap
PDF

106

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/