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Geotech VTEM-ZTEM : Airborne Acquisition Systems and Data Formats Prepared by Geoffrey Plastow ([email protected]) AEM Data Processing Manager Presented by Carlos Izarra, AEM Interpreter Collaborators: Paolo Berardelli ([email protected]) General Director of Sales & Business Development Fabiana Domingos ([email protected]) Manager of Operations in Brasil WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM/ZTEM Survey Design Defining the survey area and airborne geophysical survey. Ideally contain minimal culture – power lines, houses, pipelines, other current or ongoing geophysical surveys ground or airborne. Absent of major bodies of water (salt or fresh water). Safety concerns flying over large bodies of water. Salt Water Masks EM. Line direction – Typically flown perpendicular to Geological strike to ensure maximum coverage of Geological contacts which in mining exploration are sometimes associated with mineral occurrences. Can be determined from local / regional geological or geophysical maps. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM System Results of a TEM sounding: Voltage decay (blue) and apparent specific resistivity (red) as a function of time after switchoff of the primary field Source: BGR TEM sounding and interpretation. Source: BGR WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM System WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM Survey Design The footprint – or the surface area of the earth that will be energized will be approximately be 200-250 meters. Line Spacing – Exceeding 250 meters may potentially leave gaps or generate issues with the visualization of the survey data. Traditionally flown with 100-200 meter line space to ensure complete coverage for modeling and interpretation. Survey altitude – As the system is an active TEM system, we must induce a primary EM field into the earth. The higher from ground level the system is the less energy penetrates into ground. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM Survey Design • Severe or rugged topography may pose a challenge for any airborne survey. • • Topography may impact the survey: – Sensor altitude (above ground level, a.g.l). Inconsistent line-linetie intersections resulting in inconsistent earth response or signal levels. – Personnel safety above 10,000 ft asl. Oxygen deprivation. – Decreased survey speeds, decreased production Terrain analysis required (strongly adviced) before survey design. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM Survey Design Consider pre-planned drape surface to obtain safe consistent speed and sensor height. Can be used to predict potential sensor height agl in any topography. Important to use high resolution topographic data to generate drape surface. Aim for 30 m sensor agl in flat, 45 m in hills and 65 in rugged terrain. Airspeed should be around 80 km/h. Depending on topography +/- 20km/h WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 Loose-Drape Tight-Drape WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM Instrument Calibration High Altitude Calibration – 2,000-2,500 ft system altitude a.g.l. No earth response from system, measure only system response and or primary field. Also used to measure ideal system waveform – current waveform. The shape of the current waveform should be precisely known and measured continuously. EM receiver calibration – Coil measures an induced current / voltage so it is important to ensure the system electronics are not acting as a resistor to the measured earth response. The EM receiver should be calibrated to measure and remove the system response. EM Parallax or Lag – A conductive object – man made or geologic to correct for offset in observed data and true geographical WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 position. Ancillary Instrument Calibration • A heading test should be performed to remove any magnetic heading error associated with the direction of flight. The heading error should be less than 1.5 nT. • A radar altimeter test should be completed prior to low level survey flights. The test has two purposes: (1) To ensure the radar altimeter measures the correct altitude and increases linearly with GPS altimeter. (2) To determine the offset in altitude measuring equipment. Radar altimeter & GPS altimeter separation. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 Ancillary Instrument Calibration Airborne GPS Static Test – Recorded on the ground for 2 hours to watch instrument drift. Displayed in a scatter plot. Mean separation of points 1 m. All positional information should be post-processed using a local GPS base station. Daily forecasts of DGPS availability should be consulted. Magnetic Base station Should be within approx. 100 km of survey area and relocated during the survey to maintain this minimum distance. Sample magnetic base station data should be acquired prior to the survey for inspection and assurance no cultural influence is present in the dataset. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 Magnetic Data Processing • Synchronized with airborne data via GPS. • Lag and heading error correction. • Removal of magnetic diurnal variations. • Control line or tie line leveling. • Micro-leveling. • Visualization – 1VD, 2VD analysis. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 EM Data Processing Time Series Analysis and Field Processing Sferic Rejection EM System Response Correction EM Transient Stacking EM Time Channel Generation TDEM Processing in the Office (using Geosoft) EM Data Compensation (Background Removal) EM Filtering WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 EM Data Processing WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 Data Analysis : EM Products - Basic • Time Channel Amplitude Plots – Early, Mid, Late • Decay Constant Analysis • B Field Analysis – Suppress Overburden response. • X Coil – Fraser Filter. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 EM Products – Advanced Anomaly Picking Target Grade – Conductance Calculations Maxwell Modeling Resistivity Depth Imaging Or Conductivity Depth Imaging Depth Sections Depth Slices 1D, 2D, 3D Inversions Pattern Recognition Analysis with Magnetics WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 EM Products – Advanced South Nuqrah VTEM dBz/dt (ch30 / 880ms) with Maxwell 2.5D Plates and CVG Contours L10070 VTEM dBz/dt (0.880-7.04ms) and Maxwell 2.5D Modelling + RDI Resistivity 30siemens WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM: DELIVERABLES and FORMATS Two copies of the data and maps on DVD were prepared to accompany the report. Each DVD contains a digital file of the line data in GDB Geosoft Montaj format as well as the maps in Geosoft Montaj Map and PDF format. The survey report describes the procedures for data acquisition, processing, final image presentation and the specifications for the digital data set. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM: Geosoft GDB Data Format WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM System WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM System WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM System WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM Survey Design • Larger footprint – typically survey lines are spaced 200500m. We lose spatial resolution as we increase survey line spacing. • Less sensistive to Terrain Clearance – Due to slow fall of natural fields the ZTEM system can be flown at higher sensor altitudes relative to active EM systems. Terrain clearance is still important and should be measured and controlled. EM sensor altitude should be 80 m to 150m agl (or less). • Airspeed should be around 80 km/hr WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM Survey Design • Offer a range of frequencies from 25 Hz to 720 Hz. • A minimum of the 5 lowest frequencies should be available for surveying: 25 Hz – 360 Hz. • ZTEM base station should be within 50 km of the survey area. This ensures the a strong correlation between airborne components and ground components for tipper evaluation. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM Survey Design • Following compensation, small non-linear and low pass filters are applied to the data. Raw + Corrected In-line (Tzx) xIP Corrected + Final Smoothed In-line (Tzx) xIP Raw + Corrected Cross-line (Tzy) yIP Corrected + Final Smoothed Cross-line (Tzy) yIP WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM: Geosoft GDB Data Format Polarity Convention DT Maps TPR Maps PR = Phase Rotation WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM Survey Design A) ZTEM 90Hz In-Phase Total Divergence B) Total Magnetic Intensity 2D 0 5km n io n io ct ct Se 5km Se 2D 0 C) ZTEM 2D INVERSION ACROSS PALEOZOIC SEDIMENTARY BASIN WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 ZTEM Products – Advanced WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 VTEM-ZTEM Pre-Survey HSE • Safe location to assemble equipment and land aircraft. Cooperation with local community. • Emergency response plan. • Helicopter Safety and Awareness training for on-site staff. WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013 Obrigado pela sua atenção À ANP, muito obrigado pelo seu convite . WORKSHOP - Métodos Não Sísmicos no BDEP, ANP. Rio de Janeiro, 2013