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红河断裂带对南海西部盆地成盆过程影响机制实验研究

张家轩 郭玲莉 张京京 陶圩 赵淑娟 王光增 李三忠

海洋地质与第四纪地质2025,Vol.45Issue(2):79-97,19.
海洋地质与第四纪地质2025,Vol.45Issue(2):79-97,19.DOI:10.16562/j.cnki.0256-1492.2024020101

红河断裂带对南海西部盆地成盆过程影响机制实验研究

Red River Fault Zone affected the formation of basins in the western South China Sea:An experimental study

张家轩 1郭玲莉 1张京京 1陶圩 1赵淑娟 1王光增 1李三忠1

作者信息

  • 1. 深海圈层与地球系统教育部前沿科学中心,海底科学与探测技术教育部重点实验室,中国海洋大学海洋地球科学学院,青岛 266100||青岛海洋科技中心海洋矿产资源评价与探测技术功能实验室,青岛 266237
  • 折叠

摘要

Abstract

The strike-slip movement of the Red River Fault Zone(RRFZ)affected the formation of the basin in the western part of the South China Sea(SCS)to a certain degree.To characterize the tectonic features of the RRFZ during the uplift interval of the Tibetan Plateau and analyze the relationship between the strike-slip in RRFZ and the basins,especially Yinggehai Basin and Zhongjiannan Basin in the western SCS,sandbox analogue modelling experiments were performed in the context of the India-Eurasia collision.Results indicate that the prototypes of the two basins are controlled by the NW-oriented shear stresses generated by the strike-slip movement of the RRFZ,and the SN-oriented tensional stresses with the SCS opening up and the basin sizes expanding.During the early formation stage of the two basins,the displacement due to the strike-slipping was absorbed by the boundary faults and internal faults of the basins,thus controlling the evolution of the basins during the stage from 35 to 23 Ma.

关键词

物理模拟/成盆动力学/红河断裂带/莺歌海盆地/中建南盆地

Key words

analogue modelling/basin formation dynamic/Red River Fault Zone/Yinggehai Basin/Zhongjiannan Basin

分类

海洋学

引用本文复制引用

张家轩,郭玲莉,张京京,陶圩,赵淑娟,王光增,李三忠..红河断裂带对南海西部盆地成盆过程影响机制实验研究[J].海洋地质与第四纪地质,2025,45(2):79-97,19.

基金项目

崂山实验室科技创新项目"基于数字孪生的全球深时地貌重塑与资源环境预测"(LSKJ202204400) (LSKJ202204400)

国家自然科学基金创新研究群体项目"海底古地貌重建"(42121005) (42121005)

国家自然科学基金重大计划重点支持项目(92058211) (92058211)

李三忠教授泰山学者攀登计划项目(tspd20210305) (tspd20210305)

邢会林教授泰山学者特聘专家计划项目(tstp20221112) (tstp20221112)

海洋地质与第四纪地质

OA北大核心

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