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EXPERTISE BEYOND THE SURFACE – Take your exploration to the next level with our ground-based geophysics services. 


MASW

MASW stands for Multichannel Analysis of Surface Waves. It is used to determine the shear-wave velocity (Vs) profile of the subsurface. The principle of MASW is based on the analysis of surface waves generated by seismic sources and recorded by a linear array of geophones.

Key Advantages:
•Non-Invasive Precision: Unlike intrusive drilling methods, seismic refraction minimizes environmental disturbance while providing detailed and accurate subsurface information.
•Efficient Data Acquisition: The method allows for the rapid collection of high-quality data, facilitating timely decision-making in various applications.
•Comprehensive Imaging: MASW delivers comprehensive images of near-surface geological structures, enabling accurate interpretation and modeling for a range of projects.

Applications:
•Site Characterization
•Geotechnical Investigations
•Environmental Studies
•Infrastructure Integrity


Refraction

Seismic refraction is used to investigate subsurface structures, typically for mapping the depth and velocity of subsurface layers. The principle of seismic refraction is based on the fact that seismic waves change their direction and velocity as they encounter different geological materials with varying elastic properties.

Key Advantages:
•Non-Invasive Precision: Unlike intrusive drilling methods, seismic refraction minimizes environmental disturbance while providing detailed and accurate subsurface information.
•Cost-Effective Analysis: The acquisition of valuable geological data comes at a fraction of the cost compared to extensive drilling campaigns, making it an economically choice.
•High-Resolution Imaging: Seismic refraction provides images of subsurface structures, facilitating planning and decision-making across various industries.

Applications:
•Geotechnical Engineering
•Environmental Studies
•Mineral Exploration
•Civil Engineering


Downhole

In a seismic downhole survey, a specialized geophone sensor is lowered into a borehole drilled into the Earth's crust. Controlled seismic waves are then generated at the surface, and the resulting reflections and refractions are detected by the downhole geophone. This process allows for highly detailed subsurface imaging, capturing nuances that might be missed by surface-based seismic surveys.

Key Advantages:
•High-Resolution Imaging: The method provides exceptionally high-resolution images of subsurface structures, enabling detailed analysis and interpretation.
•Depth Penetration: Seismic downhole surveys offer increased depth penetration compared to surface-based methods, making them particularly effective in investigating deep subsurface structures.
•Improved Signal Quality: By being closer to the source of seismic energy, downhole sensors capture clearer signals, resulting in superior data quality and accuracy.

Applications:
•Geothermal Exploration
•Civil Engineering Projects
•Site Characterization
•Geotechnical Investigations


Ground-penetrating radar (GPR)

The principle of Ground-Penetrating Radar (GPR) involves emitting electromagnetic waves into the subsurface. These waves interact with subsurface materials, causing reflections based on differences in dielectric properties. The reflected signals are then detected, recorded, and analyzed. The travel times and amplitudes of these signals are used to create images of subsurface features.

Key Advantages:
•Non-Destructive Precision: GPR is a non-invasive technique that allows for detailed subsurface investigation without disturbing the ground, making it ideal for heritage sites and environmentally sensitive areas.
•Real-Time Data Acquisition: GPR provides real-time data, enabling on-site decision-making and immediate adjustments to survey parameters.
•High-Resolution Imaging: The technology delivers high-resolution images of subsurface structures, providing a comprehensive view of the geological features.

Applications:
•Archaeological Investigations
•Civil Engineering
•Environmental Monitoring
•Utility Locating
•Geological Surveys


EM31-EM61

EM surveys operate on the fundamental principles of electromagnetic induction. In these surveys, a transmitter coil generates a primary electromagnetic field that induces secondary currents in conductive subsurface materials. Receivers measure the secondary electromagnetic responses, allowing for the creation of detailed conductivity maps.

Key Advantages:

•Non-Invasive Methodology: EM surveys are non-destructive and offer a minimally invasive means of investigating subsurface conditions without disturbing the environment.
•Rapid Data Acquisition: The technology allows for efficient data collection over large areas, making it a time-effective solution for subsurface mapping.
•High Sensitivity to Conductivity Changes: EM surveys exhibit high sensitivity to variations in subsurface conductivity, providing detailed information about geological and environmental structures.

Applications:
•Environmental Site Assessments
•Unexploded Ordnance (UXO) Detection
•Mineral Exploration
•Groundwater Exploration
•Archaeological Investigations


Electrical resistivity tomography (ERT)

The principle of Electrical Resistivity Tomography (ERT) involves measuring electrical resistivity variations in the subsurface using electrodes. By injecting current and measuring voltages, ERT creates images that depict changes in resistivity, helping identify subsurface features like water, rocks, or voids.

Key Advantages:
•Non-Invasive Precision: ERT excels as a non-destructive method, offering detailed subsurface information without disturbing the natural environment.
•High Spatial Resolution: The technology provides high-resolution images of subsurface structures, providing an understanding of geological and environmental features.
•Depth Penetration: ERT has the capability to probe significant depths, making it suitable for both shallow and deep subsurface investigations.

Applications:
•Geological Investigations
•Environmental Assessments
•Hydrogeological Studies
•Civil Engineering Projects
•Archaeological Surveys


Vertical Electrical Soundings (VES)

In a VES, a series of electrodes are arranged in a linear array, with a current electrode and potential electrodes set at varying distances. A controlled electrical current is introduced into the ground, and the resulting potential differences are measured. By analyzing the relationship between current and potential, valuable data on subsurface resistivity distributions are obtained.

Key Advantages:
•Depth Profiling: VES allows for profiling subsurface resistivity at various depths, providing a comprehensive view of the electrical structure beneath the Earth's surface.
•Site-Specific Analysis: The method can be tailored to the specific needs of each site, allowing for a nuanced and detailed investigation based on the geological and environmental context.
•Quantitative Data: VES provides quantitative data on subsurface resistivity, enabling rigorous analysis and interpretation for geological and environmental studies.

Applications:
•Hydrogeological Studies
•Geotechnical Investigations
•Environmental Assessments


Magnetotelluric

In Magnetotelluric surveys, natural electromagnetic fields generated by solar wind interactions with the Earth are measured at the surface. Variations in the frequency-dependent electrical conductivity of subsurface materials induce variations in the measured electric and magnetic fields. Through careful analysis, valuable information about the electrical resistivity distribution beneath the Earth's surface can be extracted.

Key Advantages:
•Depth Profiling: MT surveys offer the ability to probe subsurface structures at various depths, providing a comprehensive understanding of geological features.
•Large-Scale Coverage: The method allows for large-scale surveys, offering extensive coverage of geological features and enabling regional-scale investigations.
•Non-Invasive Nature: MT surveys are non-intrusive, allowing for detailed subsurface investigation without disturbing the natural environment.

Applications:
•Oil and Gas Exploration
•Geothermal Exploration
•Earthquake Hazard Assessment
•Mineral Exploration
•Groundwater Studies


Magnetometry

The principle of magnetometry involves measuring variations in the Earth's magnetic field using magnetometers. Subsurface materials with different magnetic properties create anomalies. By mapping these anomalies, magnetometry helps identify features like archaeological structures or ore bodies.

Key Advantages:
•Non-Invasive Precision: Magnetometry excels in providing detailed subsurface information without the need for disruptive excavation, ensuring minimal impact on the environment.
•Efficiency in Surveying: Magnetometry surveys efficiently cover expansive areas, offering a cost-effective means of obtaining high-quality subsurface data within a reasonable timeframe.
•High Sensitivity: The technology's sensitivity allows for the detection of subtle magnetic variations, contributing to the creation of high-resolution subsurface images.

Applications:
•Archaeological Investigations
•Mineral Resource Exploration
•Environmental Assessments
•Infrastructure Analysis
•Geological Mapping


Gravimetry

Gravitational surveys operate on the principle that variations in subsurface density lead to corresponding changes in gravitational attraction. Precise measurements of gravitational acceleration are taken at the Earth's surface, providing a nuanced dataset. This data is then processed and analyzed to create detailed gravity anomaly maps, offering insights into subsurface geological structures.

Key Advantages:
•Non-Invasive Precision: Gravitational surveys are non-intrusive, allowing for detailed subsurface investigation without the need for drilling or excavation.
•Broad Depth Penetration: The method offers insights into subsurface structures at various depths, providing a comprehensive understanding of geological features.
•Global Applicability: Gravitational surveys can be conducted across diverse terrains, making them applicable to a wide range of geological settings and exploration scenarios.

Applications:
•Mineral Resource Exploration
•Geological Mapping
•Environmental Studies
•Civil Engineering Projects