利用遥感和重力数据整合划定地质结构:印度尼西亚北摩鹿加岛哈尔马赫拉的一项研究

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY VIETNAM JOURNAL OF EARTH SCIENCES Pub Date : 2024-01-25 DOI:10.15625/2615-9783/20010
P. U. Aprina, Djoko Santoso, S. Alawiyah, Nugroho Prasetyo, Khalil Ibrahim
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引用次数: 0

摘要

哈尔马赫拉岛是印度-澳大利亚板块、摩鹿加海板块和菲律宾板块相互作用的结果,由此产生了许多活跃的地质结构,在岛屿周围容易发生地震活动。这种地质结构的复杂性使得哈尔马赫拉岛非常值得研究。本研究旨在通过整合遥感和重力卫星数据来确定地质结构。使用遥感方法对地表线状结构进行分析是基于哨兵-1A 图像数据。重力法利用 GGMPlus 卫星数据来明确地表无法清晰绘制的地质结构的连续性。重力数据的线状分析使用了快速西格玛边缘检测(FSED)和欧拉解卷积等技术。基于遥感和重力卫星数据整合的线状解释结果表明,东北-西南结构控制着哈尔马海拉岛的北臂和东北臂。相比之下,南臂则由西北-东南结构控制。欧拉深度估算显示,哈尔马海拉岛地区拥有不同深度的地质结构。深层结构达 4 千米,浅层结构最深达 2 千米。地震次中心数据加强了对这一地质结构的解释。这项综合研究表明,重力和遥感技术在描述该地区的总体结构框架方面具有很好的相关性。新发现是哈尔马赫拉臂北部有一个东北-西南走向的地质结构,这可能是由两种不同的构造造成的:第一,摩鹿加海板块与西部的哈尔马赫拉板块发生俯冲。其次,由于推力断层与西侧菲律宾板块的旋转运动,北臂和东北臂被切割成东北-西南走向的走向滑动运动。
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Delineating geological structure utilizing integration of remote sensing and gravity data: a study from Halmahera, North Molucca, Indonesia
Halmahera Island is the result of the interaction between the Indo-Australian Plate, the Molucca Sea Plate, and the Philippine Plate, which gave rise to many active geological structures that are vulnerable to seismic activity around the island. The complexity of this geological structure makes Halmahera Island very interesting to study. This study aims to identify geological structures by integrating remote sensing and gravity satellite data. Surface lineament analysis using the remote sensing method was carried out based on Sentinel-1A imagery data. The gravity method uses GGMPlus satellite data to clarify the continuity of geological structures that cannot be clearly mapped on the surface. Lineament analysis on gravity data uses techniques such as fast sigmoid edge detection (FSED) and Euler deconvolution. The results of lineament interpretation based on integrating remote sensing and gravity satellite data show that the NE-SW structure controls the northern and northeastern arms of Halmahera. In contrast, the southern arm is dominated by the NW-SE structure. The Euler depth estimation shows that the Halmahera area contributes to having geological structures at various depths. Deep structures reach 4 km, while shallow structures are found at depths of up to 2 km. Earthquake hypocenter data strengthen the interpretation of this geological structure. This comprehensive study yields an excellent correlation between gravity and remote sensing techniques in describing the general structural framework of the area. The new finding is an NE-SW trending geological structure on the northern Halmahera arm, which may be caused by two different tectonics first, the subduction of the Molucca Sea Plate with the Halmahera Plate in the west. Second, the strike-slip movement is trending NE-SW, which cuts the northern and northeastern arms due to the rotational movement of the thrust fault with the Philippine Plate to the west.
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来源期刊
VIETNAM JOURNAL OF EARTH SCIENCES
VIETNAM JOURNAL OF EARTH SCIENCES GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
20.00%
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0
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