The　establishment　and　application　of　＇tectonic　deformation　lithofacies＇　mapping　highlight　the　direction　for　deep　and　peripheral　prospecting　in　old　mining　areas.　In　practice,　this　approach　has　achieved　remarkable　results　and　needs　to　be　promoted　and　further　studied.　The　understanding　of　the　deep　structure　of　tectonic　deformation　lithofacies　zone　depends　on　the　interpretation　of　geophysical　information.　Similar　to　the　properties　of　the　geophysical　field,　the　tectonic　deformation　lithofacies　zone　is　also　an　existing　geological　body.　The　purpose　of　geophysical　exploration　is　to　explore　and　reveal　the　features　of　the　burial　depth,　contour　and　internal　structure　of　the　tectonic　deformation　facies　belt,　so　as　to　provide　a　basis　for　determining　its　formation　time　and　evolutionary　process.　Due　to　the　complex　spatiotemporal　correlation　between　geological　and　geophysical　scales,　it　is　difficult　to　improve　the　resolution　and　effectiveness　of　geophysical　method　if　only　the　difference　in　physical　parameters　of　fresh　rock　specimens　is　used　as　a　discriminant　marker.　Therefore,　it　is　necessary　to　combine　tectonic　deformation　lithofacies　into　comprehensive　interpretation,　which　can　improve　the　multidisciplinary　fusion　of　interpretation　and　deduction　results.　In　searching　the　ultimate　exploration　targets,　the　structural　ore-controlling　factor　is　needed　for　setting　up　a　three-level　classification　standard　for　tectonic　deformation　facies　belt　to　extract　the　corresponding　geophysical　information.　The　first-level　is　the　tectonic　unit　and　tectonic　stress　field　of　the　target　object　as　well　as　the　corresponding　regional　geophysical　field　characteristics,　such　as　the　extensional　tectonic　domain　with　alternative　uplift　and　concave　structures.　The　second-level　refers　to　the　ore-controlling　structural　system　of　the　target　object　and　the　corresponding　geophysical　field　characteristics　of　the　ore　field,　such　as　the　magmatic　core　complex　uplift　and　detachment　structural　system.　The　third-level　is　the　favorable　metallogenic　tectonic　location　of　the　target　object　and　the　geophysical　characteristics　corresponding　to　the　key　section,　such　as　the　contact　zone　between　intrusive　rock　and　surrounding　rock　or　the　ore-bearing　fault　zone.　In　this　paper,　the　geophysical　assemblage　information　characteristics　and　workflow　of　the　three-level　tectonic　deformation　lithofacies　belt　are　introduced　for　selected　typical　metal　deposit　types　prevalent　in　the　world,　providing　an　example　for　the　effective　application　of　geophysical　exploration　methods　in　deep　prospecting　prediction.　©　2022,　Editorial　Office　of　Earth　Science　Frontiers.　All　right　reserved.