首页|广东罗湖断裂中南段构造活动性分析

广东罗湖断裂中南段构造活动性分析

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断裂的构造活动性对区域地壳稳定性、地震与变形监测、重大工程的设计和施工等具有重大的影响.本文对罗湖断裂中南段进行地层组成与分布特征、构造变形特征等方面进行研究,结合放射性14C法和伊利石40K-39Ar法等年代学测试手段,发现自中更新世晚期以来,区内断裂带再无明显活动.罗湖断裂先后经历了早白垩世初期的韧性变形和晚白垩世末期的脆性变形,晚白垩世末期的脆性变形活动可能一直持续到古新世早期;始新世中期,罗湖断裂中南段可能又发生了一期构造活动.
Analysis of Tectonic Activity in the Central-southern Segments of the Luohu Faults,Guangdong Province
The tectonic activity of the fault zone has a significant impact on regional crustal stability,earthquake and deformation monitoring,as well as the design and construction of major projects.We focus on studying of the stratigraphic composition,distribution characteristics,and structural deformation characteristics of the central-southern sections of the Luohu Faults,and adopt chronological testing methods such as the radioactive 14C of the strata and the illite 40K-39Ar of the fault gouge,then find that there has been no obviously activity of the Luohu faults since the late Middle Pleistocene.Besides,the Luohu Faults had experienced ductile deformation in the Early Cretaceous and brittle deformation in the Late Cretaceous.The brittle deformation activity in the Late Cretaceous may have continued until the early Paleocene.In the middle Eocene,another phase of tectonic activity may have occurred in the central-southern sections of the Luohu Faults.

Luohu faultstectonic activitystructural deformation40K-39Ar method

付素蓉、唐宇、高伟、王亚辉、聂云华

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深圳市建设综合勘察设计院有限公司,广东 深圳 518029

中国电建集团贵阳勘测设计研究院有限公司,贵州贵阳 550081

中国地质大学(北京)地球科学与资源学院,北京 100083

罗湖断裂 构造活动 构造变形 40K-39Ar法

2024

华南地质
武汉地质矿产研究所

华南地质

影响因子:0.516
ISSN:1007-3701
年,卷(期):2024.40(4)