Abstract

Abstract. Geo-anomalies with complex structures in the earth's crust may be defined as preferable hydrothermal ore-forming targets. The separation and explanation of anomaly from geological background have a profound influence on the analysis of geological evolution and the ore-forming process. Usually one of the key steps to identify favorable exploration targets is to determine the threshold to separate anomaly from geological background. In this paper, the singularity theory and concentration–area (C–A) fractal method was applied in determination of the threshold of geo-anomalies. According to the thresholds, four singular maps can be each divided into two segments. Each of them is correlated to the anomaly and background of the geological objects (e.g., faults, fault intersections and contacts), which reveals that the various geo-anomalies can be characterized by the singularities. The results indicate that the local singularity method can be used to identify the weak anomalies in a low background. Logistic regression model was used to combine geo-singularity maps for mineral potential mapping, which provides a useful input for further mineral exploration in the Nanling tungsten polymetallic belt, South China.

Highlights

  • Anomalous patterns created by mineralization processes from geological background have a profound influence on are often different in terms of spatial and frequency propof thCelitpehmxrPeopclaaoaenrstsaseat.tliyoUsnissutaaolrflgyegtosenoeilsoogtfioctahdleetekevreomyluisnttieeopntshaetondthidrteehsnehtiofoolyrdeff-atftovohCorsmreleaiipbmnPalge-aatseteatrrla.t,ile1sp9r9(oC6p)he.retPniegrospecetarnaql.u,baen1t9ie9fis4cs;aetniCtoihnael nofgfo,trh2et0hs0ee3s,ipd2aet0ni0atil8fi;acnaZdthioasnopeoce-ft rate anomaly from geological background

  • Developed methods the singularity theory and concentration–area (C–A) fractal of fractal and multifractal analysis provide powerful tools method was applied in determination of the threshold of geo- to quantitatively characterize the geo-anomalies and spa

  • EartDhySnyaacresnamlnoatmetbiecedamlseiteoasct.hhAedciavcnioodrmeddianligynttaoontdtwhboeascthekgrgemrsoheuonnltdds.so,EffaotchuheErogsafienotrhgltDoeuhmglayircSinasmlyacaoospmbrst--eicmstgbieeaorlg,scto1rmu9c9pt6ulebrxe;istCyahce(rCnoghs,sen2ag00rea2tn, g2ae0l.0,o3f1; 9sCc9ah4le;ensCgihnaenntdgheZahcnaodon,tAe2xg0tt1eo1r-f; jects, whiDchiscreu-ssionsAgterberg et al, 1996; Ford and McCuaig, 2010; Zhao veals that the various geo-anomalies can be characterized by et al, 2011)

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Summary

Introduction

Anomalous patterns created by mineralization processes from geological background have a profound influence on are often different in terms of spatial and frequency propof thCelitpehmxrPeopclaaoaenrstsaseat.tliyoUsnissutaaolrflgyegtosenoeilsoogtfioctahdleetekevreomyluisnttieeopntshaetondthidrteehsnehtiofoolyrdeff-atftovohCorsmreleaiipbmnPalge-aatseteatrrla.t,ile1sp9r9(oC6p)he.retPniegrospecetarnaql.u,baen1t9ie9fis4cs;aetniCtoihnael nofgfo,trh2et0hs0ee3s,ipd2aet0ni0atil8fi;acnaZdthioasnopeoce-ft rate anomaly from geological background. Model Developmentfaults, fault intersections and diversity of lithology (Wang et Discussionsal., 2012). Quantification of those structure properties can assist in understanding the inner structure of the geo-anomalies The geo-anomaly is a geologic body or geologic body combi- that often provide clues to anomaly identification. Hydrologynataionn dthat is different from its adjacent setHtinygsdirnocloomgpoysia- nd Fault systems (e.g., faults, fault intersections) and lithosEarth Syt1is9o9nte1, ;tmeZxhtuaroe,etstarlu.c, t1u9r9e,6a; nZdhagoe,ne2t0ic07s)e.qSueepnacreaEt(iZoahnraatohnadnSrdecyCoshgit-,emtarraetifgrreaqpuheinctlcyonatcaccotms apsanpireoddubcytsenoefrgnyonrleilneeaasredgewo-itphrionceshssoerst

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