在南中国海和相邻地区的莫霍模型和构造模式的深度分布
1State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, China.
这项研究使用重力数据绘制了南中国海的莫霍维奇断层 (Moho) 深度图,揭示了它与构造单位和地结构 (如岛屿弧和盆地) 的联系.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地球科学 地球科学 地球科学
背景情况:
- 南中国海的复杂构造环境需要详细的地结构分析.
- 了解莫霍维奇不连续性 (Moho) 深度对于破译构造进化至关重要.
研究的目的:
- 研究莫霍海域深度分布及其与南海构造学模式的关系.
- 划定构造单位,并确定影响该地区结构的主要断层.
主要方法:
- 分析全张量引力梯度数据以识别断层和构造单位.
- 三维 (3D) 接口反向用于Moho深度测定,受地震数据的限制.
- 重力数据,重力梯度和3D相关图像与地震约束的合分析.
主要成果:
- 确定了17个大而深的断层,并划出了9个不同的构造单位.
- 绘制了Moho深度变化图,并总结了它们的趋势,浮雕和梯度.
- 揭示了沟沟岛弧形回弧盆地系统以及大陆,海洋和过渡地的分布.
结论:
- 重力梯度异常和3D成像与Moho深度变化相关.
- 该研究提供了对南中国海大规模地和区域结构的见解.
- 证实了在研究区域内存在各种地类型和复杂的构造系统.
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