{"id":2420,"date":"2019-10-02T19:52:06","date_gmt":"2019-10-02T19:52:06","guid":{"rendered":"https:\/\/www.gsnv.org\/shop\/airborne-hyperspectral-mineral-mapping-in-regolith-and-variably-weathered-high-grade-metamorphic-sequences-of-the-mineralized-west-pinnacles-area-broken-hill-australia\/"},"modified":"2020-02-24T18:17:32","modified_gmt":"2020-02-24T18:17:32","slug":"airborne-hyperspectral-mineral-mapping-in-regolith-and-variably-weathered-high-grade-metamorphic-sequences-of-the-mineralized-west-pinnacles-area-broken-hill-australia","status":"publish","type":"product","link":"https:\/\/www.gsnv.org\/shop\/airborne-hyperspectral-mineral-mapping-in-regolith-and-variably-weathered-high-grade-metamorphic-sequences-of-the-mineralized-west-pinnacles-area-broken-hill-australia\/","title":{"rendered":"Airborne hyperspectral mineral mapping in regolith and variably weathered high-grade metamorphic sequences of the mineralized West Pinnacles area, Broken Hill, Australia"},"content":{"rendered":"","protected":false},"excerpt":{"rendered":"
The Palaeoproterozoic high-grade metamorphic Broken Hill Block, New South
\nWales (NSW), Australia, is host to the world-class Broken Hill Pb-Zn-Ag orebody. To
\nassist mineral exploration in the Block, the NSW Department of Mineral Resources
\ncommissioned a 4,000 km\u00b2 HyMap airborne hyperspectral survey in 2002 to provide
\nindustry with data capable of mapping the spectrally identifiable surface mineralogy.
\nThis paper reports on an evaluation of five HyMap flight-lines at 3 m spatial resolution,
\ncovering 48 km\u00b2 of mixed outcrop and regolith in the West Pinnacles area, 15 km
\nsouthwest of the Broken Hill orebody. A new \u2018multi MNF adapted ENVI-Hourglass\u2019
\nmethod was used to process the multiple HyMap flight-lines. Thirteen minerals were
\nidentified from the processing and analysis of the airborne data and their distribution
\nand relative abundance were mapped in the regolith and in outcrop.
\nMineral map products generated from the HyMap data proved potentially useful
\nfor mineral exploration in several ways. Many bedrock units were able to be delineated,
\nincluding retrograde shear zones. The prospective garnet- and gahnite-bearing
\nrock units were not uniquely identified, possibly due to surface weathering and\/or
\nsmall outcrop size, however, detrital garnets in stream sediments were identified. Ferich
\nfacies within prospective lithological units were detected and mark potential sites
\nof concealed mineralization. Regolith mineral distribution, relative mineral abundance,
\nprovenance, and dispersion pathways were revealed for the first time. In situ
\nand transported regolith were distinguished based predominantly on the spectrally
\ndetermined kaolin crystallinity index. Potential sampling media for geochemical analysis
\nwere mapped, including goethitic lag for Pb-Zn exploration and pedogenic calcrete
\n(calcite) for Au exploration.<\/p>\n","protected":false},"featured_media":4188,"comment_status":"closed","ping_status":"closed","template":"","meta":{"pmpro_default_level":""},"product_cat":[154],"product_tag":[],"_links":{"self":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product\/2420"}],"collection":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/comments?post=2420"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media\/4188"}],"wp:attachment":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media?parent=2420"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_cat?post=2420"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_tag?post=2420"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}