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- W83430345 abstract "The interplay of structure and Paleozoic stratigraphy is the dominant control on geometry, style, and intensity of mineralization and alteration on the Goldstrike property. Although high angle faults have long been recognized as the principal feeder structures, other subsidiary structural features exert profound control on mineralization. Compressional Antler and post-Antler deformational events have developed thrust faults and asymmetric folds observed in the field at a variety of scales. Thrust faults acted as barrier to ascending hydrothermal fluids, and mineralization is enhanced within the hinge zones of northwest trending map scale antiforms. The thrusts are intruded by Jurassic and younger felsic dikes which commonly show evidence of post emplacement deformation. Northwest striking high angle faults predate gold mineralization and are the dominant conduits for hydrothermal fluid transport. These of receptive carbonate units, and are the locus of areally extensive collapse brecciation. These structures are cut by northeast striking high angle faults which record both strike- and dip-slip displacement and provided additional conduits for fluids, particularly along structural intersections." @default.
- W83430345 created "2016-06-24" @default.
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- W83430345 date "1993-04-01" @default.
- W83430345 modified "2023-09-27" @default.
- W83430345 title "Structural controls on mineralization at the Goldstrike property, Elko and Eureka Counties, Nevada" @default.
- W83430345 hasPublicationYear "1993" @default.
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