GENERATING BOUGUER ANOMALY MAP FROM AIRBORNE GRAVITY DATA (A CASE STUDY IN SOUTH EAST SULAWESI)

L. M. Sabri, B. Sudarsono, J. Jamal, Sonny Mawardi
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引用次数: 2

Abstract

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, but the data must be carefully treated and extracted into observational gravity data. This study aims to improve the accuracy of gravity airborne data to produce an accurate complete Bouguer anomaly map. The data used in this study were airborne gravity data over Province of Southeast Sulawesi collected on September 29, 2008 to October 1, 2008.  Variation in flight height at the time of consecutive data introduced new horizontal acceleration vector. It must be treated as a noise in the measurement of gravity data. The first stage of processing was to eliminate noise due to aircraft acceleration. Gravity data measured in aircraft conditions accelerating more than 5 m.s-2 were eliminated. In this stage, the gravity data were reduced from 64481 observation points to 4900 observation points. The second stage of processing was low pass filtering to eliminate the remaining surges in gravity data. Airborne gravity data that have been snooped and filtered were then applied to calculate the complete Bouguer anomaly. Visually, a complete Bouguer anomaly map through the enhancement process produced a finer map compared to maps from airborne gravity data without enhancement. Comparison of airborne Bouguer anomaly map and terrestrial Bouguer anomaly maps of Kendari sheet showed a correlation of more than 83%. The conclusion of this study was that the enhancement of the airborne data significantly increases the accuracy and reliability of the airborne gravity data for generating a complete bouguer anomaly map. The results of this study also indicated that the airborne archive data has the potential to be used for geophysical and geosciences purposes in Southeast Sulawesi and Indonesia.
利用航空重力数据生成布格异常图(以苏拉威西岛东南部为例)
地面测量可以提供精确的重力数据,但对于大而偏远的地区,成本高且耗时长。自2008年以来,丹麦技术大学(DTU)与地理空间信息局(BIG)合作,在印度尼西亚进行了空中重力测量。该项目的目的是开发一个大地水准面模型,用于将指向椭球面的GPS/GNSS测量的高程转换为指向海平面的正测高程。实际上,这些数据可以用于地球物理和其他地球科学目的,但这些数据必须经过仔细处理,并提取为观测重力数据。本研究旨在提高重力航空数据的精度,生成准确完整的布格异常图。本研究使用的数据是2008年9月29日至2008年10月1日苏拉威西省东南部的航空重力数据。连续数据时飞行高度的变化引入了新的水平加速度矢量。在测量重力数据时,必须把它当作噪声来处理。处理的第一阶段是消除飞机加速产生的噪音。在加速超过5毫秒-2的飞机条件下测量的重力数据被删除。在这一阶段,重力数据从64481个观测点减少到4900个观测点。处理的第二阶段是低通滤波,以消除重力数据中剩余的浪涌。然后应用已被探测和过滤的航空重力数据来计算完整的布格异常。从视觉上看,与没有增强的航空重力数据相比,通过增强过程获得的完整的布格异常图产生了更精细的地图。对比Kendari片板的航空布格异常图与陆地布格异常图,相关性大于83%。本研究的结论是,航空数据的增强显著提高了航空重力数据生成完整布格异常图的精度和可靠性。本研究的结果还表明,航空档案数据具有用于苏拉威西岛东南部和印度尼西亚的地球物理和地球科学目的的潜力。
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