Item talk:Q272596
From geokb
{
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The magnetic susceptibly models derived from the electromagnetic data and the tilt derivative of the magnetic data image layering, mafic dikes, banded iron formation, and serpentinised peridotite. Known areas with contact-type mineralisation are generally characterised by low resistivities and susceptibilities where the volume of mineralised rock is large and/or the depth is shallow. We use iso-cluster and edge detection analysis of both resistivities and susceptibilities to identify potential mineralisation in poorly characterised regions as well as faults. Low resistivity layers beneath large landslides reflect water saturated porous slip surfaces which can interfere with drilling. This uncommon approach of tightly linking the resistivity and susceptibility models and magnetic anomaly data to rock property, surficial geologic, drill hole and soil geochemistry data to image the geology in the upper \u223c100\u2009m, aids identification of prospective mineralised regions as well landslides and faults that can impact mineral exploration and local hazards.", "description": "18 p.", "publisher": { "@type": "Organization", "name": "Taylor and Francis" }, "author": [ { "@type": "Person", "name": "Finn, Carol A.", "givenName": "Carol A.", "familyName": "Finn", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6178-0405", "url": "https://orcid.org/0000-0002-6178-0405" }, "affiliation": [ { "@type": "Organization", "name": "Geology, Geophysics, and Geochemistry Science Center", "url": "https://www.usgs.gov/centers/gggsc" } ] }, { "@type": "Person", "name": "Zientek, Michael L.", "givenName": "Michael L.", "familyName": "Zientek", 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