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    <Abstract>This web service delivers the geographical extents and descriptive metadata of geophysical datasets from all surveys conducted or managed by Geoscience Australia and its predecessor agencies, as well as from State and Territory geological survey agencies. Datasets include gravity, magnetic, radiometric, and electromagnetic data, and elevation data collected during geophysical surveys.</Abstract>
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    <AccessConstraints>© Commonwealth of Australia (Geoscience Australia) 2019. This product is released under the Creative Commons Attribution 4.0 International Licence</AccessConstraints>
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      <Abstract>This web service provides descriptions of geophysical surveys and datasets derived from those surveys, which are delivered by the Geophysical Archive Data Delivery System v2.0 (https://www.geoscience.gov.au/gadds).</Abstract>
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        <Title>Geophysical Survey Datasets - Airborne Electromagnetics</Title>
        <Abstract>Airborne Electromagnetic (AEM) data are used in minerals, energy, and groundwater resource exploration. The AEM technique takes advantage of natural variations in electrical conductivity beneath the surface, which results from variation in rock and pore fluid properties. The presence of electrically conductive minerals such as graphite, clays, and sulfide minerals, or electrically conductive fluid such as saline groundwater, results in greater conductivity relative to non-conductive mineral assemblages, or non-conductive fluid (typically fresh ground water).&#13;
&#13;
AEM data are collected by transmitting an electromagnetic signal from a system attached to a plane or helicopter. The signal induces eddy currents in the ground which are detected by receiver coils towed below and behind the aircraft. &#13;
&#13;
Precompetitive AEM data and associated scientific analysis assists exploration under cover by reducing risk, stimulating investment and promoting exploration for commodities. In recent years, Geoscience Australia has flown Airborne Electromagnetic (AEM) surveys across regional Australia. Data and associated interpretations from such regional surveys have led to tenement take up, stimulated exploration for a number of commodities.</Abstract>
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        <Abstract>Digital Elevation data record the terrain height variations from the processed point-located data recorded during a geophysical survey. The data acquired are a mass of ground heights representing a terrain surface. The data are either geoidal (representing the vertical distance from a location on the Earth's surface to the geoid) or ellipsoidal (representing the vertical distance from a location on the Earth's surface to the ellipsoid). The data are given in units of meters. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.</Abstract>
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        <Abstract>Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. Once processed and enhanced, magnetic data can be used to locate structural features such as dykes and faults. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose</Abstract>
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        <Abstract>The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). Radiometrics can tell us about the distribution of certain soils and rocks. Geologists and geophysicists routinely use it as a geological mapping tool to tell them where certain rock types change. It is also useful for the study of geomorphology and soils. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.</Abstract>
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        <Abstract>Descriptions of geophysical datasets, their associated surveys, and the methods used for delivery of those datasets.  Includes datasets collected from airborne, land, and marine surveys conducted or managed by Geoscience Australia and its predecessor agencies, as well as data and surveys from State and Territory geological survey agencies</Abstract>
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        <KeywordList>
          <Keyword>geophysics</Keyword>
          <Keyword>geophysical survey</Keyword>
          <Keyword>magnetism</Keyword>
          <Keyword>radiometrics</Keyword>
          <Keyword>gravity</Keyword>
          <Keyword>electromagnetics</Keyword>
          <Keyword>elevation</Keyword>
          <Keyword>airborne survey</Keyword>
          <Keyword>ground survey</Keyword>
          <Keyword>marine survey</Keyword>
          <Keyword>GADDS</Keyword>
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          <Title>Geophysical Surveys</Title>
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