FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2399686814> ?p ?o ?g. }

• W2399686814 endingPage "1098" @default.
• W2399686814 startingPage "1073" @default.
• W2399686814 abstract "Gold mineralization at the Ballarat East deposit, central Victoria, Australia, is hosted in lodes that are historically known as “leather jackets.” These are quartz-dominant vein arrays related to low-displacement, W-dipping faults (≤45°) that transect the core and/or eastern limb of tight, asymmetric N-S-trending anticlines. The leather jacket lodes typically have dip extents from 5 to 65 m, widths of ≤20 m, and strike lengths up to hundreds of meters, but their along-strike continuity is disrupted by oblique, low-displacement listric faults known as “cross courses.” The gold lodes are characterized by distinct phases of sulfide paragenesis with minor gold + arsenopyrite + pyrite defining the early sulfide stage. Late-stage coarse gold was precipitated with galena + sphalerite ± pyrrhotite ± chalcopyrite (late pyrite also occurs). The gold mineralization events are linked to low-strain mineralized fracture networks, which are closely related to the final deformation stages and the amplification of the major folds enclosing the lodes. This amplification produced domal fold culminations, with plunges ≤30°, and localized minor parasitic folds with shallower plunges (≤10°). A network of dilation sites, on the W-dipping faults, preferentially developed in the cores of anticlines, particularly in zones where there are changes in strike of bedding or fault bifurcation and refraction through contrasting sandstone and interbedded packages of sandstone and shale.Numerical three-dimensional simulations were undertaken to test our geologic observations and replicate conditions controlling the emplacement of the leather jacket lodes. Two different scenarios were investigated: first, to determine how changes in the local stress field orientation influences dilation and fluid infiltration; secondly, to test variations in fault geometry during the last stages of deformation—that is, within the final 2% of shortening, when most of the mineralized sites were created. Results show that strain and fluid flow localized along refracted sections of faults and around changes in dip, specifically on the shallower dipping sections within subvertical sandstone units. This is consistent with the observation that high-grade gold-bearing quartz is associated with localized changes in fault dip in thicker sandstone and sandstone-shale packages. There was also a component of strike-slip motion and near-field NW-to-SE or N-to-S stress fields, which can be attributed to the development of a component of out-of-plane motion during the development of fold culminations. The preferred model for the distribution of the high-grade auriferous vein arrays defining the leather jacket lodes is one of fold amplification and extension parallel to the fold axes, which produced an increasing out-of-plane relaxation. The main fluid conduits responsible for the leather jacket style of mineralization involve infiltration along steep bedding-parallel faults and veins that link up with the arrays of low-displacement W-dipping faults." @default.
• W2399686814 created "2016-06-24" @default.
• W2399686814 creator A5033136304 @default.
• W2399686814 creator A5048584901 @default.
• W2399686814 creator A5064708553 @default.
• W2399686814 creator A5091704716 @default.
• W2399686814 date "2016-05-23" @default.
• W2399686814 modified "2023-10-14" @default.
• W2399686814 title "Structural Constraints and Localization of Gold Mineralization in Leather Jacket Lodes, Ballarat, Victoria, Australia" @default.
• W2399686814 cites W1513455127 @default.
• W2399686814 cites W1748073762 @default.
• W2399686814 cites W1963667046 @default.
• W2399686814 cites W1965756128 @default.
• W2399686814 cites W1966335995 @default.
• W2399686814 cites W1972088733 @default.
• W2399686814 cites W1980947043 @default.
• W2399686814 cites W1998030007 @default.
• W2399686814 cites W2025821781 @default.
• W2399686814 cites W2046180871 @default.
• W2399686814 cites W2046517367 @default.
• W2399686814 cites W2046590164 @default.
• W2399686814 cites W2048620508 @default.
• W2399686814 cites W2049028113 @default.
• W2399686814 cites W2050971615 @default.
• W2399686814 cites W2051795001 @default.
• W2399686814 cites W2055588902 @default.
• W2399686814 cites W2067458423 @default.
• W2399686814 cites W2071320029 @default.
• W2399686814 cites W2074894858 @default.
• W2399686814 cites W2080604186 @default.
• W2399686814 cites W2112525731 @default.
• W2399686814 cites W2148302241 @default.
• W2399686814 cites W2154295153 @default.
• W2399686814 cites W2161994868 @default.
• W2399686814 cites W2165197944 @default.
• W2399686814 cites W2169162133 @default.
• W2399686814 cites W2485952619 @default.
• W2399686814 cites W71764628 @default.
• W2399686814 cites W2187626893 @default.
• W2399686814 doi "https://doi.org/10.2113/econgeo.111.5.1073" @default.
• W2399686814 hasPublicationYear "2016" @default.
• W2399686814 type Work @default.
• W2399686814 sameAs 2399686814 @default.
• W2399686814 citedByCount "21" @default.
• W2399686814 countsByYear W23996868142016 @default.
• W2399686814 countsByYear W23996868142017 @default.
• W2399686814 countsByYear W23996868142018 @default.
• W2399686814 countsByYear W23996868142019 @default.
• W2399686814 countsByYear W23996868142020 @default.
• W2399686814 countsByYear W23996868142021 @default.
• W2399686814 countsByYear W23996868142022 @default.
• W2399686814 countsByYear W23996868142023 @default.
• W2399686814 crossrefType "journal-article" @default.
• W2399686814 hasAuthorship W2399686814A5033136304 @default.
• W2399686814 hasAuthorship W2399686814A5048584901 @default.
• W2399686814 hasAuthorship W2399686814A5064708553 @default.
• W2399686814 hasAuthorship W2399686814A5091704716 @default.
• W2399686814 hasBestOaLocation W23996868142 @default.
• W2399686814 hasConcept C111696902 @default.
• W2399686814 hasConcept C127313418 @default.
• W2399686814 hasConcept C159390177 @default.
• W2399686814 hasConcept C159750122 @default.
• W2399686814 hasConcept C17409809 @default.
• W2399686814 hasConceptScore W2399686814C111696902 @default.
• W2399686814 hasConceptScore W2399686814C127313418 @default.
• W2399686814 hasConceptScore W2399686814C159390177 @default.
• W2399686814 hasConceptScore W2399686814C159750122 @default.
• W2399686814 hasConceptScore W2399686814C17409809 @default.
• W2399686814 hasIssue "5" @default.
• W2399686814 hasLocation W23996868141 @default.
• W2399686814 hasLocation W23996868142 @default.
• W2399686814 hasOpenAccess W2399686814 @default.
• W2399686814 hasPrimaryLocation W23996868141 @default.
• W2399686814 hasRelatedWork W1758497512 @default.
• W2399686814 hasRelatedWork W1996097370 @default.
• W2399686814 hasRelatedWork W2036099453 @default.
• W2399686814 hasRelatedWork W2040829098 @default.
• W2399686814 hasRelatedWork W2083430702 @default.
• W2399686814 hasRelatedWork W2361911732 @default.
• W2399686814 hasRelatedWork W2380934447 @default.
• W2399686814 hasRelatedWork W2538103680 @default.
• W2399686814 hasRelatedWork W2996184140 @default.
• W2399686814 hasRelatedWork W2999252365 @default.
• W2399686814 hasVolume "111" @default.
• W2399686814 isParatext "false" @default.
• W2399686814 isRetracted "false" @default.
• W2399686814 magId "2399686814" @default.
• W2399686814 workType "article" @default.