Estimation of Depth of Magnetic Anomalies Using Standard Euler Deconvolution method in Talle Jar Area, Kurdistan Province
عنوان دوره: نوزدهمین کنفرانس ژئوفیزیک ایران
کد مقاله : 1513-NIGS
نویسندگان
1موسسه ژئوفیزیک، ژئوالکتریک
2دانشگاه فردوسی مشهد
3استاد/دانشگاه فردوسی مشهد
چکیده
ABSTRACT
Depth estimation of the ore anomalies in the different basins is the main goal in geomagnetic explorations. The depth estimation of this kind of anomalies can be done using different methods, in the cases where the bedrock is magnetized. In processing and interpreting ground magnetic data, the depth of buried anomaly can be calculated in several ways. In this paper, the estimation of magnetic anomalies due to magnetic scans in the Talle Jar region of Kurdistan province is investigated using Euler method. Investigations in this area, including a relatively large anomaly in the south of the region, yielded a depth of 10 to 20 m for this anomaly, which is consistent with the preliminary results of field observations.
Depth estimation of the ore anomalies in the different basins is the main goal in geomagnetic explorations. The depth estimation of this kind of anomalies can be done using different methods, in the cases where the bedrock is magnetized. In processing and interpreting ground magnetic data, the depth of buried anomaly can be calculated in several ways. In this paper, the estimation of magnetic anomalies due to magnetic scans in the Talle Jar region of Kurdistan province is investigated using Euler method. Investigations in this area, including a relatively large anomaly in the south of the region, yielded a depth of 10 to 20 m for this anomaly, which is consistent with the preliminary results of field observations.
کلیدواژه ها
Title
Estimation of Depth of Magnetic Anomalies Using Standard Euler Deconvolution method in Talle Jar Area, Kurdistan Province
Authors
Mohammad Ali Shahrabi, Masoud Doustzadeh, Naser Hafezi Moghaddas
Abstract
ABSTRACT
Depth estimation of the ore anomalies in the different basins is the main goal in geomagnetic explorations. The depth estimation of this kind of anomalies can be done using different methods, in the cases where the bedrock is magnetized. In processing and interpreting ground magnetic data, the depth of buried anomaly can be calculated in several ways. In this paper, the estimation of magnetic anomalies due to magnetic scans in the Talle Jar region of Kurdistan province is investigated using Euler method. Investigations in this area, including a relatively large anomaly in the south of the region, yielded a depth of 10 to 20 m for this anomaly, which is consistent with the preliminary results of field observations.
Depth estimation of the ore anomalies in the different basins is the main goal in geomagnetic explorations. The depth estimation of this kind of anomalies can be done using different methods, in the cases where the bedrock is magnetized. In processing and interpreting ground magnetic data, the depth of buried anomaly can be calculated in several ways. In this paper, the estimation of magnetic anomalies due to magnetic scans in the Talle Jar region of Kurdistan province is investigated using Euler method. Investigations in this area, including a relatively large anomaly in the south of the region, yielded a depth of 10 to 20 m for this anomaly, which is consistent with the preliminary results of field observations.
Keywords
Keywords: Magnetic method, Euler deconvolution, Talle Jar