在库里尔-卡姆查特卡地区使用更新的全球潜水带热结构重新估计板块脱水面
Weiling Zhu1,2, Yingfeng Ji1,2, Lijun Liu3
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
iScience
|July 31, 2023
概括
更温暖的俯冲板块解释了前弧热流和岩石状况的差异. 这种精细的热模型将板块变暖与脱水阵线联系起来,驱动快速和缓慢的俯冲地震.
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:
- 降温热模型与前弧热流 (50-140 mW/m2) 发生冲突.
- 挖掘的岩石P-T条件表明,比预测的200-300°C更温暖的浅层环境.
- 现有的模型无法将热异常和潜伏区的地震观测相协调.
研究的目的:
- 用3D热力学模拟重新评估潜伏热模型.
- 为了研究库里尔-卡姆查特卡地区的潜水板的热状态.
- 了解板块热异常与地震发生之间的联系.
主要方法:
- 潜伏的3D热力学建模.
- 纳入观察到的沉降历史和板块几何.
- 分析板块的热状态和脱水过程.
主要成果:
- 精炼的3D板块的热状态比2D模型预测的要温暖.
- 更温暖的板块在各种前弧深度产生分层脱水阵线.
- 这些脱水阵线与快速和缓慢的俯冲地震的发生有关.
结论:
- 更温暖的降温板块对于理解前弧热状态至关重要.
- 较弱的脱水面被确定为地震发生的关键机制.
- 快速到缓慢的俯冲地震平衡了巨型冲击的能量释放,影响了板块的合.
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