Academic literature on the topic 'Bouguer anomaly map'

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Journal articles on the topic "Bouguer anomaly map"

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Maulana, Aji Darma, and Aprilia Frinanda Setiawan. "PENINGKATAN AKURASI COMPLETE BOUGUER ANOMALY MAP PADA DATA TOPEX SATELLITE MENGGUNAKAN KONSTANTA BARU BERDASARKAN MATHEMATICAL DERRIVATIVE." JURNAL TEKNIK GEOLOGI : Jurnal Ilmu Pengetahuan dan Teknologi 5, no. 2 (2023): 22. http://dx.doi.org/10.30872/jtgeo.v5i2.5463.

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Penelitian dilakukan dengan menggunakan data gravitasi observasi satelit TOPEX dengan luas area sebesar 37.530 km2 berupa Free Air Anomaly. Penelitian berbasis analisis ini berlandaskan ketidaksesuaian antara dinamika geologi dengan data pengolahan gravitasi conventional. Dengan menekankan pada pengolahan gravitasi secara unconventional, analisis ini bertujuan untuk mendapatkan besaran yang dapat mereduksi efek topografi tanpa menghilangkan informasi litologi. Pengolahan dilakukan dengan cara membandingkan beberapa variasi perlakuan koreksi Bouguer pada nilai Free Air Anomaly. Perlakuan terseb
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Keating, Pierre. "Interpretation of the gravity anomaly field in the Noranda – Val d'Or region, Abitibi Greenstone Belt, Canadian Shield." Canadian Journal of Earth Sciences 29, no. 5 (1992): 962–71. http://dx.doi.org/10.1139/e92-080.

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Gravity data from the Noranda – Val d'Or region have been reprocessed: the Bouguer anomaly map, the first vertical derivative map, and an apparent density map have been used for geological interpretation of the gravity field in this region. It is found that variations in the Bouguer anomaly can be mainly explained by density structures located within the uppermost 5 km of the crust. The vertical derivative map helps to better locate some geological contacts, and the apparent density map allows the easy distinction between thin and thick batholiths. Generalized inversion was used to calculate d
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Ilmi, Nasyratul, and Karyanto Karyanto. "PEMODELAN 3D STRUKTUR BAWAH PERMUKAAN GUNUNGAPI AGUNG PROVINSI BALI MENGGUNAKAN METODE GAYA BERAT." Jurnal Geofisika Eksplorasi 5, no. 2 (2020): 68–75. http://dx.doi.org/10.23960/jge.v5i2.30.

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Under surface structure, 3d modelling of Agung volcano in Bali had been conducted by using gravity methods. This research aims to identify the magma chamber and make a model below the surface of the Great Volcano of Bali Province by using gravity anomaly data. Data processing methods performed in this research were consists of six steps: (i) arrangement the contour map of Bouguer anomaly, (ii) spectrum analysis, (iii) anomaly regional and residual separation, (iv) Second Vertical Derivative analysis, (v) cross-section of subsurface geology construction by using 3D (inverse modelling), (vi) qua
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Gunawan, Hendra, Micheldiament Micheldiament, and Valentin Mikhailov. "Estimation of Bouguer Density Precision: Development of Method for Analysis of La Soufriere Volcano Gravity Data." Indonesian Journal on Geoscience 3, no. 3 (2008): 151–59. http://dx.doi.org/10.17014/ijog.3.3.151-159.

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http://dx.doi.org/10.17014/ijog.vol3no3.20084The precision of topographic density (Bouguer density) estimation by the Nettleton approach is based on a minimum correlation of Bouguer gravity anomaly and topography. The other method, the Parasnis approach, is based on a minimum correlation of Bouguer gravity anomaly and Bouguer correction. The precision of Bouguer density estimates was investigated by both methods on simple 2D syntetic models and under an assumption free-air anomaly consisting of an effect of topography, an effect of intracrustal, and an isostatic compensation. Based on simulati
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Al Shida Natul and Leni Sophia Heliani. "A Comparison of Geologic Structure Detection of Sumatera Island Using Goce Satellite Gravity Data and Sgg-Ugm-2 Data." Journal of Geoscience, Engineering, Environment, and Technology 7, no. 3 (2022): 95–101. http://dx.doi.org/10.25299/jgeet.2022.7.3.8863.

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GOCE gravity satellite data can be used for regional fault detection because the observation area is wide and not limited by area. In this study, GOCE satellite data is used to detect geological structures on the island of Sumatra, the results of which are used as the basis for disaster mitigation. GOCE data and SGG-UGM-2 were processed using the GOCE User Toolbox (GUT) software to produce a gravity disturbance map and a complete bouguer anomaly map. The GOCE obtained results were validated using the SGG-UGM-2 high-resolution gravity model data. The calculation results obtained that the gravit
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Threza, Imelda, Winardi Tjahyo Baskoro, Ida Bagus Alit Pramarta, I. Ketut Sukarasa, Putu Suardana, and I. Wayan Supardi. "IDENTIFIKASI STRUKTUR BAWAH PERMUKAAN BERDASARKAN DATA ANOMALI GRAVITASI DI PULAU LOMBOK." Kappa Journal 8, no. 1 (2024): 120–29. https://doi.org/10.29408/kpj.v8i1.25139.

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Abstract: Research on the identification of subsurface structures based on gravity anomaly data on Lombok Island. This research aims to create a map and determine the value of the complete Bouguer anomaly, regional anomaly, residual anomaly, subsurface density value and create a 2-D model of the subsurface structure. The data used is secondary data, namely satellite gravity anomaly data obtained from the topex website. Data processing in this research uses the gravity method. In this method, gravity correction will be carried out, making a complete bouguer anomaly map, conducting spectrum anal
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Siombone, Salman Hamja, Adi Susilo, and Sukir Maryanto. "Integration of Topex Satellite Gravity and DEM SRTM Imagery for Subsurface Structure Identification at Tiris Geothermal Area, Lamongan Volcano Complex, Probolinggo, East Java." POSITRON 12, no. 2 (2022): 98. http://dx.doi.org/10.26418/positron.v12i2.56880.

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Tiris area is one area that has geothermal prospects. Tiris area is located in the Tiris sub-district, Probolinggo regency, East Java. This study aims to identify the subsurface structure of the Tiris geothermal area using Topex gravity and DEM SRTM imagery data. The Topex gravity data obtained is still in Free Air Anomali (FAA) form, so it is necessary to make Bouguer and terrain corrections to get a complete Bouguer anomaly. A residual Bouguer anomaly is needed to study shallow subsurface structures. This anomaly is obtained by separating the residual and regional anomalies from the complete
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Sabri, Laode M., Bambang Sudarsono, Jamal Jamal, and Sonny Mawardi. "GENERATING BOUGUER ANOMALY MAP FROM AIRBORNE GRAVITY DATA (A CASE STUDY IN SOUTH EAST SULAWESI)." Elipsoida : Jurnal Geodesi dan Geomatika 3, no. 02 (2020): 151–56. http://dx.doi.org/10.14710/elipsoida.2020.9213.

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Terrestrial measurements can provide accurate gravity data, but it is costly and time-consuming for large and remote area. Airborne gravity measurements have actually been carried out in Indonesia since 2008 by Technical University of Denmark (DTU) in collaboration with the Geospatial Information Agency (BIG). Purpose of the project was to develop a geoid model used for converting elevations from GPS/GNSS measurements that refers to ellipsoid to orthometric elevations that refer to sea level. The data can actually be explored so that it can be used for geophysical and other geoscience purposes
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Medved, Klemen, Oleg Odalović, and Božo Koler. "New Bouguer Anomaly Map for the Territory of the Slovenia." Remote Sensing 13, no. 22 (2021): 4510. http://dx.doi.org/10.3390/rs13224510.

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The existing Bouguer anomaly map, which covers the territory of the Republic of Slovenia is a few decades old. Since then, quite a few new gravimetric measurements (data) for the territory of Slovenia as well as high quality digital terrain models that are needed for creating such a map have been made available. The methodology and standards for creating gravity anomaly maps are also changing. Thus, the national Bouguer anomaly map was updated. There were some gross errors detected in the set of old gravimetric data. Additionally, the influence of new updated gravimetric data was analyzed. The
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Sihombing, Roy Bryanson, and Rustadi Rustadi. "PEMODELAN DAN ANALISA STRUKTUR BAWAH PERMUKAAN DAERAH PROSPEK PANASBUMI KEPAHIANG BERDASARKAN METODE GAYABERAT." Jurnal Geofisika Eksplorasi 4, no. 2 (2020): 47–61. http://dx.doi.org/10.23960/jge.v4i2.14.

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Research has been conducted in Kepahiang area using gravity data with the aim of identify faults based on analysis of the Second Vertical Derivative (SVD) and interpreting structure sub-surface of the based on 3D inverse modelling from Bouguer anomaly and residual anomaly. The research area have an Bouguer anomaly between 38 mGal - 74 mGal, where the high Bouguer anomaly value has a value range of 63,2 mGal - 74 mGal located in the southwest direction of the research area. Whereas the low Bouguer anomaly value has a range of values 38 mGal - 47 mGal located in the north of the research area. T
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Books on the topic "Bouguer anomaly map"

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Kevi, L. Dinninup 1:100 000: Bouguer anomaly map. Geological Survey of Western Australia, 1991.

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Kevi, L. The Quongering Gravity Low: 1:100000 Bouguer anomaly map. Geological Survey of Western Australia, 1992.

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M, Kulik D., and Geological Survey (U.S.), eds. Gravity survey data and a Bouguer gravity anomaly map of southwestern Wyoming, northeastern Utah, and northwestern Colorado. U.S. Dept. of the Interior, Geological Survey, 1985.

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M, Kulik D., and Geological Survey (U.S.), eds. Gravity survey data and a complete Bouguer gravity anomaly map of southwestern Wyoming, northeastern Utah, and northwestern Colorado. U.S. Dept. of the Interior, Geological Survey, 1989.

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Complete bouguer gravity anomaly map of Utah. Utah Geological Survey, 1989. http://dx.doi.org/10.34191/m-122.

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Project, Mid-Norden. Gravity anomaly map of central Fennoscandia: Bouguer anomalies. Mid-Norden Project, 1996.

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Project, Nordkalott. Gravity anomaly map, northern Fennoscandia: Terrain corrected Bouguer anomalies. Nordkalott Project, 1986.

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Tully, M. C., and J. A. Donato. 1:1 000 000 Northern North Sea Bouguer Anomaly Gravity Map (BGS Reports). Stationery Office Books, 1985.

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Complete Bouguer gravity anomaly map and geological interpretation of the southern Wasatch Front, Utah. Utah Geological Survey, 1997. http://dx.doi.org/10.34191/cr-97-1.

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Smith, I. F. Colour Shaded Relief Gravity Anomaly Map of Britain, Ireland, and Adjacent Areas: Land Areas--Bouguer Anomaly, Sea Areas--Free Air Anomaly (1:1 500 000 Series). British Geological Survey, 1997.

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Book chapters on the topic "Bouguer anomaly map"

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Abubakar, Adamu, and Othniel K. Likkason. "Exploring the Application of Potential Field Gravity Method in Characterizing Regional-trends of the Earth’s Sequence System over the Sokoto Basin, NW, Nigeria." In Earth's Crust and its Evolution - From Pangea to the Present Continents [Working Title]. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.102940.

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In this chapter some preliminaries evaluation were outline briefly based on exploring the use of potential gravity field method in characterizing regional trends of Earth’s sequence system interms of gravitational potentials and fields, viz-a-viz., the background, instrumentation, theoretical model, gravity data reduction, geological framework, Bouguer reduction density, density acceptable models, free-air anomaly and interpretation of Bouguer gravity anomaly. Therefore, application of potential field method (gravity) explore these relationships by focusing on the formation and fill of a conti
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Kane, M. F., and R. H. Godson. "5. Features of a Pair of Long-Wavelength (>250 km) and Short-Wavelength (<250 km) Bouguer Gravity Maps of the United States." In The Utility of Regional Gravity and Magnetic Anomaly Maps. Society of Exploration Geophysicists, 1985. http://dx.doi.org/10.1190/1.0931830346.ch5.

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Conference papers on the topic "Bouguer anomaly map"

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Adib, Adib, Radhiyullah Armi, Sabrian Tri Anda, and Azwanda Azwanda. "Evaluating the Reliability of Satellite Gravity Data for Disaster Risk Mapping in West Coast Aceh's Coal Mines." In The 2nd International Conferences on Applied Engineering, Science, Technology and Innovation. Trans Tech Publications Ltd, 2025. https://doi.org/10.4028/p-bgmz9u.

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This study evaluates the accuracy of satellite gravity methods in disaster risk mapping for the coal mining areas of West Coast Aceh, specifically between longitudes 96.00°E to 96.30°E and latitudes 4.00° to 4.30°. The satellite gravity technique was utilized to detect fault zones through the examination of rock density variations. The collected data was processed to determine the complete Bouguer anomaly, including terrain corrections based on an initial average density of 2.67 g/cm³. The complete Bouguer anomaly values span from -36.2 mGal to 42.4 mGal, with higher values concentrated in the
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Xu, Menglong, Changbao Yang, and Yangang Wu. "A study on the separation of a Bouguer anomaly map using wavelet analysis." In International Conference on Earth Science and Environmental Protection (ICESEP2013). WIT Press, 2013. http://dx.doi.org/10.2495/icesep130231.

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Rodríguez, Pablo, Josefina Marmisolle, Pablo Gristo, Héctor de Santa Ana, and Gerardo Veroslavsky. "Bouguer anomaly map and 2D modeling case study from Santa Lucía Basin, onshore Uruguay." In SEG Technical Program Expanded Abstracts 2020. Society of Exploration Geophysicists, 2020. http://dx.doi.org/10.1190/segam2020-3426365.1.

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Rodríguez*, Pablo, Gerardo Veroslavsky, Matías Soto, et al. "New integrated Bouguer gravity anomaly map onshore Uruguay: preliminary implications for the recognition of crustal domains." In SEG Technical Program Expanded Abstracts 2015. Society of Exploration Geophysicists, 2015. http://dx.doi.org/10.1190/segam2015-5821993.1.

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Bakkali, Saad. "Application of the Automatic Optimal Spline Smoothing Method to Optimizing Edges of Moroccan Bouguer Gravity Anomaly Map." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2011. Environment and Engineering Geophysical Society, 2011. http://dx.doi.org/10.4133/1.3614159.

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Filho, Walter Malagutti, Maximilian Fries, João Carlos Dourado, and Mariana Aparecida Fernandes. "Gravimetric study in the northeast portion of Paraná Sedimentary Basin – Southeast Brazil. A preliminary Bouguer anomaly map." In 9th International Congress of the Brazilian Geophysical Society & EXPOGEF, Salvador, Bahia, Brazil, 11-14 September 2005. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2005. http://dx.doi.org/10.1190/sbgf2005-146.

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Malagutti Filho, Walter, Maximilian Fries, João Carlos Dourado, and Mariana Aparecida Fernandes. "Gravimetric study in the northeast portion of Paraná Sedimentary Basin – Southeast Brazil. A preliminary Bouguer anomaly map." In 9th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.160.sbgf146.

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Masinde, Abiud, Cleophas Simiyu, Innocent Murunga, George Muia, Aaron Waswa, and Justus Barongo. "A Preliminary Assessment of the Hydrocarbon Potential of Kerio Valley Basin: Gravity and Magnetic Interpretation." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2546156-ms.

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ABSTRACT The aim of the study was to assess the hydrocarbon prospectivity of the Kerio Basin in the Kenya Rift. An Isostatically corrected anomaly map produced from a Bouguer anomaly grid was filtered using a Hanning low pass filter of order 2 to remove low wavelengths. Four profiles were extracted from the grid to give 1D interpretation along straight lines. Magnetic grid was corrected for IGRF, diurnal, filtered using a 1 Hz low pass 10km Hanning filter to reduce noise, later, reduced to equator to place all anomalies directly over underlying sources and make anomalies less complicated. Tilt
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Yanis, Muhammad, Zaini Nasrullah, Muhammad Isa, Ananda Riski, Muzakir Zainal, and Andri Yadi Paembonan. "Optimizing the Gravity Data and Geological Observation for Mapping the Local Fault around the Jaboi Volcano." In The 5th International Conference on Science and Technology Applications. Trans Tech Publications Ltd, 2024. http://dx.doi.org/10.4028/p-mezta6.

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Geothermal is a very expensive investment industry. Therefore, it is necessary to map a geological structure in the sub-surface, i.e., faults, and rock formations that control volcanic hydrothermal systems to reduce investment risk in the exploitation of geothermal. On the other hand, the hydrothermal system aims for flow paths connecting reservoir wells for fluid production. The Jaboi Volcano, with an estimated 80 MWe located on Weh Island, Indonesia, has been planned by the government to develop electrical energy, where the excess energy will be exported to Banda Aceh via undersea cables. We
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Soupios, Pantelis, Alexandros Stampolidis, Maurizio Fedi, et al. "Gravity Survey of King Fahd University of Petroleum and Minerals Dammam Dome, Saudi Arabia." In SPE Middle East Oil & Gas Show and Conference. SPE, 2021. http://dx.doi.org/10.2118/204564-ms.

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Abstract The study area is a part of Dammam Dome that is situated at King Fahd University of Petroleum &amp; Minerals (KFUPM) campus, Dhahran, Kingdom of Saudi Arabia. The gravity survey was conducted as a pilot case study to explore part of Dammam Dome in greater detail. Gravity data were collected solely during night hours due to low noise levels. A significant part of the survey was conducted during the summer holiday period, , when there was no student are on campus. A total of 235 gravity measurements were made using a Scintrex CG5 gravitometer, while a Trimble R10+ differential GPS (DGPS
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Reports on the topic "Bouguer anomaly map"

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Goodacre, A. K., R. A. F. Grieve, and J. F. Halpenny. Bouguer gravity anomaly map of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/127245.

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Cook, D. G., and B. C. MacLean. Figure 6. Bouguer gravity anomaly map (free air offshore). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/216180.

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Goodacre, A. K., R. A. F. Grieve, and J. F. Halpenny. Horizontal gradient of the Bouguer gravity anomaly map of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/127247.

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Goodacre, A. K., R. A. F. Grieve, and J. F. Halpenny. Vertical gradient of the Bouguer gravity anomaly map of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127671.

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Pilkington, M., R. A. F. Grieve, J. D. Rupert, and J. F. Halpenny. Vertical gradient of the Bouguer gravity anomaly map of North America. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/183809.

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Pilkington, M., R. A. F. Grieve, J. D. Rupert, and J. F. Halpenny. Horizontal gradient of the Bouguer gravity anomaly map of North America. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/183810.

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Oakey, G. N., R. Forsberg, and H. R. Jackson. Gravity anomaly map, bouguer on land, free air at sea, Innuitian region, Canadian and Greenland Arctic. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212064.

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Morris, R., D. M. Jobin, M. D. Thomas, N. Rogers, and S R McCutcheon. New gravity data for the Bathurst Mining Camp, northeastern New Brunswick: a colour-shaded Bouguer gravity anomaly map (linear colour contour interval) with gravity station locations and posted Bouguer anomaly values. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223792.

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Oakey, G. N., R. Forsberg, and H. R. Jackson. Gravity anomaly map, bouguer on land, free air at sea, Labrador Sea region, Canadian and Greenland Arctic. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212060.

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Oakey, G. N., R. Forsberg, and H. R. Jackson. Gravity anomaly map, bouguer on land, free air at sea, Davis Strait region, Canadian and Greenland Arctic. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212061.

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