PEMODELAN DUA DIMENSI (2D) BAWAH PERMUKAAN PULAU ADONARA DENGAN DATA ANOMALI GRAVITASI

K. K. Lesu, Jehunias Leonidas Tanesib, Bernandus Bernandus
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Abstract

Geophysical research has been carried out using the gravity method on Adonara island in east Flores Regency, East Nusa Tenggara. This study aims to determine the subsurface rock geological conditions of the research area using free air gravity anomaly data from GGMplus and ERTM2160. The data is reduced by atmospheric correction, simple bouguer correction, curvature correction to produce a complete bouguer anomaly. After correction, regional anomalies and residual anomalies are separated. Then 2-dimensional (2D) modeling is carried out using forward modeling and inversion modeling with Grav2DC software. The results of the study show that the subsurface geological conditions of Adonara island are dominated rock by andesite, granite, diorite, dolomite, gravel, sandstone, basalt, sekis, metamorphic, shale and lavas.
亚多尼拉岛表面以下的二维模型与重力异常数据
利用重力法在东努沙登加拉岛弗洛雷斯县东部的Adonara岛进行了地球物理研究。利用GGMplus和ERTM2160自由空气重力异常资料,确定研究区地下岩石地质条件。通过大气校正、简单的布格校正、曲率校正对数据进行简化,得到完整的布格异常。校正后将区域异常与残差异常分离。然后利用Grav2DC软件进行二维(2D)正演建模和反演建模。研究结果表明,Adonara岛地下地质条件以安山岩、花岗岩、闪长岩、白云岩、砾石、砂岩、玄武岩、sekis、变质岩、页岩和熔岩为主。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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