LEADER 04304nam 2201021z- 450 001 9910346688203321 005 20231214133652.0 010 $a3-03897-785-3 035 $a(CKB)4920000000094787 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/60142 035 $a(EXLCZ)994920000000094787 100 $a20202102d2019 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aStructural Control of Mineral Deposits. Theory and Reality 210 $cMDPI - Multidisciplinary Digital Publishing Institute$d2019 215 $a1 electronic resource (256 p.) 311 $a3-03897-784-5 330 $a""Structural Control"" remains a crucial point that frequently lacks in any scientific and/or economic analysis of ore deposits, whatever their type and class. The case of lode deposits is exemplary, although also other deposits, like breccia pipe, stockwerk, massive sulphides, skarn, etc., can, surprisingly, be concerned. Several concepts like the gold-bearing shear zone have not proven valid during the last few decades in terms of our understanding of gold deposit and have been totally abandoned. Additionally, the relationships between magmatism, regional tectonic context, and mineralization remain uncertain and have been debated in several recent publications. This demonstrates that this issue is still relevant, and its solution may help in the distinction between intrusion-related and orogenic deposits. In this Special Issue, we particularly invite any case study of mineral deposits, in which it has been demonstrated that structural geology may have a significant role in the establishment of the deposit model of formation and/or on exploration and exploitation programs. Examples in which the structural model diverges from those described in the classical literature are particularly welcomed, including studies in which relationships with magmatism can be suspected and/or demonstrated. Indeed, all cases that illustrate concepts that differ from the classic ones and from theoretical models may represent significant contributions to this volume. 610 $ashallow diagenesis 610 $aarsenopyrite 610 $abuffer-based analysis 610 $avein-filling 610 $atextures 610 $ahydrothermal breccia 610 $aPyrenean Axial Zone 610 $aTibet 610 $aremobilization 610 $apull-apart 610 $aspatial analysis 610 $atectonic control 610 $athrust fault 610 $asilicic large igneous province 610 $ahinge trap 610 $ahydraulic breccia 610 $avein 610 $aexploration 610 $amafic dikes 610 $aTiegelongnan 610 $aorogenic gold mineralization 610 $aporphyry 610 $abase metal massive sulfide deposits 610 $aoverprinting 610 $adeformation bands 610 $aclay authigenesis 610 $afractal 610 $auranium deposits 610 $areplacement 610 $asphalerite 610 $aTongling 610 $acomb quartz 610 $astrike-slip fault 610 $apre-existing structures 610 $apreservation 610 $aignimbrite flare-ups 610 $adilational jogs 610 $aPb-Zn deposits 610 $adeformation structure 610 $asilicification 610 $aSEDEX 610 $afault zones 610 $aVerkhoyansk-Kolyma folded region 610 $adecollement 610 $astructural control 610 $aIRGD 610 $aKhangalas ore cluster 610 $ainfilling 610 $abreccia 610 $alate Variscan strike-slip faults 610 $adata-driven model 610 $amineralization chronology 610 $ashear zone 610 $aepithermal 610 $astructure 610 $aHajjar 610 $aorogenic gold 610 $aKiggavik 610 $asulphide lenses 610 $aAnti-Atlas 610 $aash-flow caldera 700 $aChauvet$b Alain$4auth$0268363 906 $aBOOK 912 $a9910346688203321 996 $aStructural Control of Mineral Deposits. Theory and Reality$93036520 997 $aUNINA