geophysical methodsThere are a variety of geophysical survey methods that are used both in mineral prospecting or regional mapping. Using either ground or airborne techniques, geophysical companies employ the use of magnetic, radiometric and electromagnetic equipment to detect concentrations of minerals in the Earth's crust.
 
Magnetic Surveys:
 
The most commonly used geophysical survey method is the aeromagnetic survey, in which a magnetometer is either attached to an aircraft on a stinger or towed behind on a long line to measure the intensity of the earth's magnetic field, thereby permitting the detection of ambient magnetic fields caused by the minerals that are present in the ground. The separation of the magnetic sensor from the aircraft is critical to the quality of the data, hence the need for specially modified aircraft for geophysical exploration.
 
The resolution of the data is dependent upon, among other things, the distance between the traverse line spacing and, as such a survey can be categorized as either regional or detailed.
 
A regional survey is measured in Line kilometers, which is the distance that the aircraft must travel to cover the entire survey area flying in a grid pattern. Typically a regional survey is an area of at least 5000 Lkm with a traverse line spacing of at least 250 meters or more.
 
A detailed aeromagnetic survey, as the name suggests, offers data at a higher resolution and can be used as a means of direct prospecting by mining companies, typically performed at 50m meters line spacing and as low and slow to the ground as is possible within the safety parameters of the aircraft (30-50m AGL). A detailed survey will offer improved data on the presence of economic minerals and for mapping geology and structure.
 
There are two basic approaches to the application and interpretation of magnetic data: direct and indirect exploration. Many economic minerals are either themselves magnetic creating a characteristic magnetic field which can be detected by a survey or they may be intimately associated with or hosted by minerals or rock types that possess a magnetic signature. In these cases these economic minerals can be identified directly by magnetic surveys; this allows the mining companies to progress rapidly to ground based, detailed exploration and delineation of the resource.
 
In the case of indirect exploration, the magnetic data are used to map the geology and structure in far greater detail than is available by the ground mapping of outcrops which are commonly separated by large areas of overburden. Once the detail of the stratigraphy and structure has been improved, the geologist is then able to other apply types data (eg geochemistry, drilling, seismic, etc.) to enhance the predictability of geologic modeling. This procedure models all observed data with the known characteristics of different types of economic mineral deposits in order to detect any similarities and thereby identify any new potential mineralization. For example, hydrocarbons themselves are not magnetic, but information about the surrounding geology may be modeled to identify a typical depositional environment for the potential accumulation and entrapment of hydrocarbons.
 
Radiometric Surveys:
 
Terraquest primarily uses airborne digital, gamma-ray spectrometers which are designed for the detection and measurement of low-level radiation from both naturally occurring and man-made sources, associated with the radioactive elements thorium, potassium, and uranium. Gamma Ray Spectrometry provides a direct measurement of the surface of the earth, with no significant penetration, but permits reliable measurement of the radioactive element contacts to the mapped bedrock and surficial geology. (Source: www.nrcan.gr.ca)
 
Potassium (K), uranium (U) and thorium (Th) are the three most abundant, naturally occurring radioactive elements. K is a major constituent of most rocks and is the predominant alteration product in many mineral deposits. Uranium and thorium are present in trace amounts, as mobile and immobile elements, respectively. As the concentration of these different radioactive elements varies between different rock types, we can use the information provided by a gamma-ray spectrometer to map the rocks. Where the 'normal' radioelement signature of the rocks is disrupted by a mineralizing system, corresponding radioelement anomalies provide direct exploration guidance. (Source; www.nrcan.gr.ca)
 
Airborne radiometric methods provide detailed, systematic coverage of large areas which are invaluable to improving the mapping, especially when used in conjunction with other survey products such as magnetics.
 
Electromagnetic Surveys:
 
Electromagnetic surveys (EM) are designed to measure the conductivity in the surface of the earth in either a "target mode” for identifying conductive minerals such as graphite or massive sulphides (base metal minerals) or in a "mapping mode” to identify long conductive structures. The successfulness of electromagnetic surveys is impaired in geological environments where the country rock is highly conductive or where the overburden is both thick and conductive.
 
There are two types of EM surveys, active and passive. Active EM requires the utilization of a powerful source to transmit a local electromagnetic field (referred to as the primary field) from the aircraft. This field penetrates the ground and ideally energizes conductors within the bedrock, which in turn generate weaker secondary fields. The airborne survey measures both primary and secondary fields but through processing, the secondary field can be enhanced.
 
There are two modes of active EM surveys, frequency domain and time domain. The frequency domain system utilizes different frequencies to identify different EM characteristics of the ground conductor. The time domain system uses a pulse transmitter and the EM characteristics are identified according to the decay of the signal strength.
 
The second type, passive EM utilizes natural (eg AFMAG) and/or more commonly, existing man made sources (VLF) to energize the conductors. The VLF signal is transmitted around the world by governments, primarily for communication purposes. In North America there are three transmitters, a very powerful one in Cutler, Maine (24.0 KHz) another of medium power at LaMoure, North Dakota (25.2 KHz) and another at Jim Creek, Washington (24.8) Signals from these transmitters cover most of the continent and act as primary fields that are capable of energizing conductive bodies (such as graphite, metallic minerals and structures) in the ground. Once energized, the current within these bodies emits a secondary field forming the basis for a geophysical exploration.
 
Terraquest uses a recently developed proprietary method of measuring Very Low Frequency (VLF) EM, called XDS VLF-EM to map structure. The XDS VLF-EM system uses three orthogonal coils mounted in the aircraft stinger, coupled with a broadband receiver to record all frequencies between 22.0-27.0 KHz (to include all three North American VLF stations), to measure separately the X, Y and Z components of the VLF field. Continuous monitoring of all three, combined VLF frequencies reduces the reliance on any one transmitter during periodic maintenance downtime. Individual three-axis component data provides more detailed information about the nature of the earth's conductivity than simple total field measurements could, primarily because the coils respond differently to different conductors. The horizontal components tend to be strongest where currents are present (over conductive zones) while the z component tends to peak over contacts.
 
The system typically responds to variations in overburden conductivity, to large faults or shear zones, and to graphitic formational conductors. Because of these characteristics, XDS VLF-EM can be useful as a mapping tool, particularly when combined with magnetics.
 
Summary:
 
The combination of magnetic data with gamma-ray spectrometry and electromagnetic data, in a modern digital system, yields powerful mapping and exploration tools for both direct and indirect exploration techniques for economic minerals for mining companies.
 
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geophysical methods of exploration
Geophysical methods of exploration are means to collect geophysical data that can be used to prospect directly for economic minerals that are characterized by anomalous magnetic, conductive or radiometric responses.
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Geophysical survey methods are becoming more sophisticated and accurate. There are many airborne and ground methods that can be used separately or combined to produce the most accurate data possible .
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A geophysical company is capable of acquiring precise data regarding valuable minerals that are located under the Earth’s surface. Geophysical companies also offer sufficient means of acquiring information used in geophysical map development.
geophysical methods
Geophysical methods of conducting airborne surveys are used by mining companies as a means of efficient mineral prospecting. Through the use of aeromagnetic, radiometric and electromagnetic surveys, it is possible to identify areas that contain high concentrations of economic minerals that characterized by changes in geophysical responses.
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Advances in technology are allowing the geophysical survey system industry to thrive by making these systems smaller, more accurate and easier to implement.
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Geophysical survey companies are pushing innovation and coming up with new technologies and methods to more accurately identify targets and map geological structure from the air surveying. Geophysical surveys are an integral part of the mineral exploration process.
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Terraquest Ltd.        |        9054772800        |        sb@terraquest.ca        |        www.terraquest.ca
2-2800 John Street,   Markham,   ON,   L3R 0E2,   Canada