西藏波密地区深部密度结构与地震活动的关系
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1.昆明理工大学国土资源工程学院;2.中国地质科学院地质研究所

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国家自然(42174123)和国家自然(41941016)联合资助。


Relationship between deep density structure and seismic in Bomi area of Tibet
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1.昆明理工大学国土资源工程学院;2.Institute of Geology ,Chinese Academy of Geological Sciences;3.Institute of Land and Resources Engineering Kunming University of Science and Technolody

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    摘要:

    西藏波密地区位于南迦巴瓦构造结东北部,是研究喜马拉雅东构造结演化的关键地区,同时也是我国“十四五”期间重点交通项目--川藏铁路项目的必经之路,因此研究其深部地质结构导致的稳定性和安全性具有重要意义。但受地质地貌条件限制,该地区地球物理资料匮乏,因此波密地区的深部密度结构与地震的关系研究甚少。本文首次获得波密地区1:20万布格重力数据,并利用小波变换多尺度分解方法、刻痕分析方法和重力三维反演方法,获得了不同尺度的重力异常、断层分布和密度结构。结果分析表明,波密地区整体地壳密度变化明显,与断裂分布密切相关。同时结合区域地质资料,在波密地区推断了20条断裂,发现了4处较大的横向密度不均匀带,并推断了贯穿研究区的嘉黎断裂带的产状。在此基础上利用该地区地震及余震活动记录,本文分析了深部密度结构与地震的关系。通过对研究区的断裂构造、地震活动与重力异常的密度横向变化可知,该地区地震活动、断裂带与岩石密度扰动的横向不均匀性密切相关,地震主要位于密度差异带的高密度区域。最后讨论了深部密度结构对波密地区重大铁路工程-川藏铁路的潜在影响,并提出了相应建议。

    Abstract:

    The Bomi region of Tibet is located in the northeast of the Namche Barwa tectonic junction.It is a key area for studying the evolution of tectonic junctions in the eastern Himalayas.At the same time,it holds great significance for the Sichuan-Tibet Railway project, which is a key transportation initiative during the Fourteenth Five-Year Plan period. Therefore, it is crucial to study the stability and safety of the region"s deep geological structure. However, the scarcity of geophysical data in the area, due to limitations in geological and geomorphological conditions, has resulted in limited research on the relationship between deep density structure and seismic in the Bomi region.This thesis obtains 1:200,000 bouguer gravity data in Bomi region for the first time.First,we used the wavelet transform multi-scale decomposition method, scratch analysis method and gravity 3D inversion method to divide the tectonic activity unit, we obtained the gravity anomalies of different , faults distribution and density structures. The analysis results show that the overall crust density in the Bomi region changes significantly, which is closely related to the fault distribution. At the same time, combined with the regional geological data,our inferred 20 faults in the Bomi area、found 4 large transverse density uneven zones and deduced the occurrence of Jiali fault zone which runs through the study area. In addition, using the seismic and aftershock activity records in the area, analyzing the relationship between deep density structure and earthquake. Finally, according to the transverse variation of fault structure density, seismic activty and gravity anomaly in the study area, it can be seen that the seismic, fault zone and rock density disturbance are closely related to the transverse unevenness, and the earthquakes are mainly located in the high-density area of the density difference zone. Based on the above analysis, We discussed the potential influence of deep density structure on major railway projects----Sichuan-Tibet Railway in Bomi area is discussed, and corresponding suggestions are put forward.

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  • 收稿日期:2023-06-26
  • 最后修改日期:2023-10-10
  • 录用日期:2023-10-12
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