用重力总水平梯度增强法测定黄沙群岛地下轮廓

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Luan Pham Thanh, E. Oksum, O. Kafadar, Trinh Phan Trong, Dat Nguyen Viet, Quynh Vo Thanh, Sang Le Thi
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引用次数: 21

摘要

黄沙群岛位于东越南海北部,缺乏地质构造边界的信息。利用增强的总水平梯度法对全球海洋重力模型的重力数据进行分析,圈定了在转换后的重力异常图上呈现为线状的地质构造。在将该技术应用于黄沙群岛重力数据之前,通过将其与综合模型的总水平梯度方法的结果进行比较,证明了其有效性。应用增强水平梯度方法分析发现,黄沙群岛的大部分地貌走向为WSW-ENE、NE-SW、E-W、WNW-ESE和NNW-SSE方向。这些结果有助于更好地了解这些岛屿的地下构造特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determination of subsurface lineaments in the Hoang Sa islands using enhanced methods of gravity total horizontal gradient
The Hoang Sa islands, located in the northern part of the East Vietnam Sea, lack information on geological structural boundaries. The gravity data from the global marine gravity model were analyzed using the enhanced total horizontal gradient methods to delineate geological structures that appear as lineaments on the transformed gravity anomaly maps of the area. Before applying the techniques to gravity data of the Hoang Sa islands, their effectiveness was demonstrated by comparing them with the results from the total horizontal gradient method for a synthetic model. Applying the enhanced horizontal gradient methods shows that most of the lineaments identified in the Hoang Sa islands are trending in the WSW-ENE, NE-SW, E-W, WNW-ESE and NNW-SSE directions. These results provide a better understanding of the subsurface structural features of the islands.
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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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