Nuestra Misión es ofrecer la mayor variedad de métodos geofísicos para cubrir todos los tipos de depósitos minerales existentes a los mejores costos y calidad de datos. 

LEVANTAMIENTO MAGDRONE USANDO SENSORES FLUXGATE 3D DOBLES

Que Métodos Ofrecemos?

MAGNETOTELURIC METHOD (MT)

FROM NEAR THE SURFACE TO ANY DRILLING DEPTH, MT ALLOWS RAPID RECOGNITION OF AREAS AS LARGE AS TENS OF SQUARE KILOMETERS, WHILE DETECTING CONDUCTIVE AREAS 2000 M DEEP AND MORE. TIGHTLY SPACED STATIONS ALONG LINES OR MESHES PROVIDE DATA REDUNDANCY, HIGH LATERAL RESOLUTION, AND A CONTINUOUS PICTURE OF THE SUBSURFACE RESISTIVITY STRUCTURE. MT/AMT SEES THROUGH COARSE CONDUCTIVE CLAY (IMPENETRABLE BY AIRBORNE EM OR OTHER SURFACE TECHNIQUES) COVERING MANY POTENTIAL AREAS

GRAVITY MÉTHOD

THE GRAVIMETRIC METHOD IS BASED ON THE FACT THAT DIFFERENT GEOLOGICAL UNITS HAVE DIFFERENT DENSITIES, THESE BEING THE BASIC PHYSICAL PARAMETER OF THIS METHOD. A GRAVITY ANOMALY IS DEFINED AS THE DIFFERENCE BETWEEN OBSERVED GRAVITY AND THEORETICAL (OR NORMAL) GRAVITY IN THE AREA OF INTEREST AFTER THE NECESSARY CORRECTIONS HAVE BEEN APPLIED (TIDES, INSTRUMENT DRIFT, LATITUDE, HEIGHT). BECAUSE THE GRAVITY VARIATIONS ARE VERY SMALL, THE MILIGAL (MGAL) OR MICROGAL ('GAL' IS COMMONLY USED. THE CG-6 AUTOGRAV IS AN AUTOMATED GRAVITY METER THAT HAS A WORLDWIDE MEASUREMENT RANGE OF OVER 8,000 MGALS AND A READING RESOLUTION OF 0.0001 MGAL. THIS ENABLES THE USER TO OPERATE IN BOTH DETAILED MICRO-GRAVITY SURVEYS AND LARGE SCALE REGIONAL OR GEODETIC SURVEYS

VERY LOW FREQUENCY ELECTROMAGNETIC METHOD (VLF)

VLF (VERY LOW FREQUENCY) PROSPECTING METHOD USE VERY LOW FREQUENCY RADIO COMMUNICATION SIGNALS TO DETERMINE THE ELECTRICAL PROPERTIES OF SHALLOW ROCK BEDS AND NEAR-SURFACE SOILS, MAINLY AS A RECOGNITION TOOL. VLF PROFILES CAN BE RUN QUICKLY AND ECONOMICALLY TO IDENTIFY ANOMALOUS AREAS THAT WARRANT FURTHER RESEARCH BY OTHER STUDIES, PERFORATIONS, OR SAMPLING. THE TECHNIQUE IS ESPECIALLY USEFUL FOR MAPPING ABRUPT IMMERSION STRUCTURES, SUCH AS FAULTS, FRACTURES AND SHALLOW AREAS OF POTENTIAL MINERALIZATION. THE DEPTH OF RESEARCH VARIES FROM 4-5 METERS IN CONDUCTIVE SOILS TO 40-60 METERS IN HIGHLY RESISTIVE SOILS.

MAGDRONE AIRBORNE SURVEYS

THE APPLICATION OF DRONE SYSTEMS (UAVs) DEFINES A NEW DEVELOPMENT IN MAGNETIC GEOPHYSICAL STUDIES IN AREAS OF MINERAL INTEREST WITH DIFFICULT RELIEF, WHICH DO NOT ALLOW CONVENTIONAL STUDIES. THE BENEFITS OF UAV IMPLEMENTATION INCLUDE EXTENSIVE AREA COVERAGE IN SHORTER TIMEFRAMES, HIGH-RESOLUTION IMAGES, AND HIGH DATA DENSITY. FOR THESE SURVEYS, MAGNETIC SENSORS CONTROLLED BY UAVs ARE IMPLEMENTED AT A CONSTANT CONTROLLED ELEVATION WITH A GNSS CENTIMETRIC POSITIONING SYSTEM INCORPORATED INTO THE EQUIPMENT; USED TO OBTAIN THE EXACT COORDINATES ASSOCIATED WITH THE MEASUREMENTS.

INDUCED POLARIZATION IP METHOD

INDUCED POLARIZATION (IP) IS CAUSED BY AN ELECTRON TRANSFER REACTION IN AN INDUCED CURRENT BETWEEN ELECTROLYTES AND METALLIC MINERALS. THE INJECTED CURRENT IS INTERRUPTED AND THE DIFFERENCE IN POTENTIAL MEASURED DOES NOT DECAY TO ZERO INSTANTLY. THIS DECAY TIME IS IN THE ORDER OF SECONDS AND MEASUREMENTS CAN BE PERFORMED IN THE TIME DOMAIN IF THE VOLTAGE IS MEASURED BASED ON TIME. THE METHOD IS APPLIED IN THE EXPLORATION OF METALS, GROUNDWATER AND CONTAMINANTS. USING THE INDUCED POLARIZATION METHOD DETERMINE POSSIBLE MINERALIZED BODIES AT DEPTH, SINCE THIS METHOD PROVIDES US WITH TWO PARAMETERS: CHARGEABILITY, RELATED TO THE PRESENCE OF SULPHIDES; AND RESISTIVITY, RELATED TO AREAS OF ALTERATION. FROM THE DATA OBTAINED PERFORM THE INVESTMENT PROCESS IN 3D, THE RESULTS OF WHICH ALLOW US TO INFER THE THREE-DIMENSIONAL GEOMETRY OF ANOMALIES WITH GEOLOGICAL-MINERALOGICAL POTENTIAL.

DISTRIBUTED 3D IP SISTEM

• INNOVATIVE SYSTEM ON THE MARKET. THIS 3D IP SYSTEM WILL STAND OUT IN THE WORLD OF GEOPHYSICAL INDUSTRY WITH THE ABILITY TO DO QUALITY CONTROL AND ANALYSIS (QA / QC) OF THE DATA DIRECTLY IN THE FIELD FOR EACH OF THE GDD IP RECEIVER MODELS. • DISTRIBUTED IP USES THE SAME CURRENT TRANSMISSION POINT, GIVING STRONG REDUNDANCY TO THE DATA, AS WELL AS BETTER QUALITY CONTROL. THE DISTRIBUTED 3D ARRAY ALLOWS READING ALL ACTIVE POTENTIAL ELECTRODES WITH A SINGLE CURRENT INJECTION PER STATION.

VEHICULOS AEREOS NO TRIPULADOS EN MINERIA 

FOTOGRAMETRIA CON DRONES:

  1. CURVAS DE NIVEL
  2. ORTOFOTO
  3. NUBES DE PUNTOS 3D
  4. MODELOS DE ELEVACIONES DEM, DTM
  5. ESCANEO DE AREA A ALTA RESOLUCION

LIDAR

LiDAR (Light Detection And Ranging) es una tecnología que permite medir la distancia entre un sensor y un objeto, a través de un rayo de luz láser para obtener medidas de posicionamiento georreferenciadas mediante modelos digitales tridimensionales de alta precisión.