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    Geosciences Desktop Study

  • Jasa Survey Georadar GPR untuk pemetaan pipa kabel utilitas bawah permukaan Taman Mini Indonesia Indah

    GPR survey activities at the TMII were carried out to map existing utilities in their area. This survey activity requires

    a GPR antenna of 450 MHz, so that the depth and the data resolution obtained can be more optimal at less than 6-meter

    depth. Underground utilities are indicated by hyperbolic shape in radargram. A similar pattern in other radargram confirms

    the existing underground utilities.

  • Jasa Survey Georadar GPR untuk inspeksi landasan pesawat terbang Bandara Internasional Soekarno Hatta

    GPR survey activities at the Soetta Airport were carried out to confirm the injected material into the concrete road. A High-

    resolution GPR antenna of 600 MHz was utilized to scan the area to get a depth penetration of shallower than 4 meters.

    Different materials are indicated by anomalous patterns in radargram. A similar pattern in other radargrams confirms the

    existing different injected material into concrete.

  • Jasa Survey Georadar GPR untuk inspeksi retakan dinding Universitas Kristen Satya Wacana Salatiga

    A Very high-resolution GPR scanning activity at one of the UKSW buildings was carried out to assess the building wall crack.

    A GPR antenna of 1600 MHz was utilized to scan the area to get a depth penetration of shallower than 60 centimeters. A

    crack is indicated by anomalous patterns in the radargram. A similar pattern in other radargrams confirms the existing crack

    inside the wall.

  • Jasa Survey Seismik Downhole untuk penentuan kecepatan gelombang P di bawah tanah yang membantu investigasi geoteknik ketahanan tanah Lotte Chemical Cilegon

    A Seismic Downhole Test measures the shear wave velocity of the soil or rock layers. The source at the surface generates a

    seismic wave that travels through the ground and is detected by the receiver which is deployed at a borehole at different

    depths. The shear wave velocity is an indicator of the stiffness and strength of the subsurface material. The data is used

    as a consideration for an engineer to build a construction

  • Survey GPS Geodetik Penentuan koordinat titik ukur teliti pada stasiun pengamatan gravitasi dalam eksplorasi migas Lirik Riau

    Topographical Surveys that produce detailed surface contours with good precision and accuracy are needed as the main

    input for effective and efficient architectural and engineering designs. By using satellite technology and sophisticated GPS

    equipment and experts in their fields, the best topographic survey results will be realized.

  • Survey Geolistrik di situs arkeologi Batu Kalde Pangandaran

    Electric resistivity as a physical property of soil layers or rock layers is a reference in explaining the characteristics of these

    layers by injecting electric current into the earth's body and measuring the electric potential voltage that is formed. Electrical

    resistivity is a measure of the ability of rock layers to conduct electric current which is very necessary for the design of a

    surface facility which is strongly influenced by the earth's electrical activity.

  • Survey Geomagnet di Gunung Papandayan membantu proyek riset Guru Besar

    The Earth's magnetic properties can be utilized for regional geological studies, mineral exploration, geothermal exploration,

    as well as various investigative activities related to buried objects based on the element iron (Fe) using the Geomagnetic

    method. The combination of topographical information, the results of surface geological mapping, and data from the

    Geomagnetic Survey can produce the desired subsurface model to determine the steps of exploration activities.

  • Survey Gravitasi eksplorasi geotermal panas bumi Gunung Hamiding

    Gravity surveys can provide useful information for geothermal exploration, such as the depth and geometry of basins, the

    location and orientation of faults, and the presence of magma chambers. Gravity surveys are relatively inexpensive, non-

    invasive, and can cover large areas with high resolution, but has some limitations, such as the non-uniqueness of gravity

    inversion solutions, the need for accurate terrain corrections, and the influence of regional gravity anomalies.

  • Kalibrasi alat survey gravity Jalur Museum Geologi Bandung hingga Gunung Tangkuban Parahu

    Gravity Survey is applied to get an overview of the earth's subsurface model based on the distribution of rock density values

    that have a certain geometry so that it is good to do in the early stages of Exploration activities. Utilizing a gravity meter

    instrument that is capable of accurately measuring the magnitude of the gravitational field, a reliable geophysicist can

    produce a model of an oil and gas basin, a model of a geothermal system, and other earth exploration.

  • Survey Batimetri untuk pemetaan morfologi bawah laut atau sungai

    Oceanographic survey is a scientific method for collecting data and information about the oceans. Oceanographers use

    special equipment and techniques to measure and study the physical, chemical, biological and geological properties of the

    oceans, such as temperature, salinity, depth, ocean currents and the biodiversity in them. The results of oceanographic

    surveys can be used for sustainable management and marine conservation and inform marine resource management policies

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