首页|利用重力资料研究苏禄海地区断裂构造

利用重力资料研究苏禄海地区断裂构造

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为了研究苏禄海地区断裂构造特征,收集并整理了研究区的自由空间重力异常数据,利用滑动平均滤波的方法对自由空间重力异常数据进行处理,得到局部重力异常.结合前人研究成果,对研究区的自由空间重力异常和局部重力异常特征进行深入分析,探讨了研究区断裂构造分布特征.研究结果显示,研究区的重力异常有明显的分区性,大致以潘丹-锡帕莱-第波罗-拉巴松-仙那港为界,分界线南部与北部重力变化相差较大.基于重力异常特征确定了 9组不同规模的断裂带,这些断裂带主要呈北东向或北西向展布,延伸距离较长,规模较大,对苏禄海地区的构造单元的划分及部分复杂地质构造的形成起控制作用.
Fault Structure of the Sulu Sea Based on Gravity Data
In order to study the tectonic features of the Sulu Sea area,the free-space gravity anomaly data of the study area were collected,collated,and processed to obtain local gravity anomalies by using the sliding average filtering method.Combining the results of previous research,the characteristics of free-space gravity anomalies and local gravity anomalies in the study area are analyzed in depth,and the distribution characteristics of fracture tectonics in the study area are discussed.The study results show that the gravity anomalies in the study area are clearly zoned,roughly bounded by Pandan-Sipalay-Tibolo-LabassonSenna Port,with a large difference in gravity variation between the southern and northern part of the dividing line.Based on the gravity anomaly features,nine groups of fracture zones of different scales were identified,which are mainly spreading in a north-easterly or north-westerly direction,with long extension distance and large scale,and play a controlling role in the delineation of tectonic units and the formation of some complex geological structures in the Sulu Sea area.

faultstructural featuresgravity anomalySulu Sea

赵敏、张春灌、周磊、张秋屹

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西安石油大学地球科学与工程学院,西安 710065

西安石油大学陕西省油气成藏地质学重点实验室,西安 710065

西南石油大学地球科学与技术学院,成都 610500

断裂 构造特征 重力异常 苏禄海

2024

西安文理学院学报(自然科学版)
西安文理学院

西安文理学院学报(自然科学版)

影响因子:0.209
ISSN:1008-5564
年,卷(期):2024.27(2)