...
首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Crustal structure of the Eastern Alps along the TRANSALP profile from wide-angle seismic tomography
【24h】

Crustal structure of the Eastern Alps along the TRANSALP profile from wide-angle seismic tomography

机译:广角地震层析成像沿TRANSALP剖面的东阿尔卑斯山地壳结构

获取原文
获取原文并翻译 | 示例

摘要

The objective of the TRANSALP project is an investigation of the Eastern Alps with regard to their deep structure and dynamic evolution. The core of the project is a 340-km-long seismic profile at 12 degrees E between Munich and Venice. This paper deals with the P-wave velocity distribution as derived from active source travel time tomography. Our database consists of Vibroseis and explosion seismic travel times recorded at up to 100 seismological stations distributed in a 30-km-wide corridor along the profile. In order to derive a velocity and reflector model, we simultaneously inverted refractions and reflections using a derivative of a damped least squares approach for local earthquake tomography. 8000 travel time picks from dense Vibroseis recordings provide the basis for high resolution in the upper crust. Explosion seismic wide-angle reflection travel times constrain both deeper crustal velocities and structure of the crust-mantle boundary with low resolution. In the resulting model, the Adriatic crust shows significantly higher P-wave velocities than the European crust. The European Moho is dipping south at an angle of 7 degrees. The Adriatic Moho dips north with a gentle inclination at shallower depths. This geometry suggests S-directed subduction. Azimuthal variations of the first-break velocities as well as observations of shear wave splitting reveal strong anisotropy in the Tauern Window. We explain this finding by foliations and laminations generated by lateral extrusion. Based on the P-wave model we also localized almost 100 local earthquakes recorded during the 2-month acquisition campaign in 1999. Seismicity patterns in the North seem related to the Inn valley shear zone, and to thrusting of Austroalpine units over European basement. The alignment of deep seismicity in the Trento-Vicenza region with the top of the Adriatic lower crust corroborates the suggestion of a deep thrust fault in the Southern Alps. (c) 2005 Elsevier B.V. All rights reserved.
机译:TRANSALP项目的目的是对东阿尔卑斯山的深层结构和动态演化进行调查。该项目的核心是慕尼黑和威尼斯之间12点东经340公里长的地震剖面。本文讨论了从有源源传播时间层析成像中得出的P波速度分布。我们的数据库包括沿剖面分布在30公里宽走廊中的多达100个地震台站记录的震源和爆炸地震传播时间。为了导出速度和反射器模型,我们使用阻尼最小二乘法的导数同时对局部地震层析成像进行了倒置折射和反射。密集的Vibroseis记录中有8000个行程选择,为高分辨率的上地壳奠定了基础。爆炸地震的广角反射传播时间限制了较深的地壳速度和低分辨率的地幔幔边界结构。在生成的模型中,亚得里亚海地壳的P波速度明显高于欧洲地壳。欧洲莫霍面人以7度角向南倾斜。亚得里亚海的莫霍面以较平缓的倾斜向北倾斜,深度较浅。这种几何形状暗示了S向俯冲。初速的方位角变化以及对剪切波分裂的观察表明,在陶恩窗中存在强烈的各向异性。我们通过横向挤压产生的叶片和薄片来解释这一发现。基于P波模型,我们还对1999年为期2个月的采集活动中记录的近100次本地地震进行了定位。北部的地震模式似乎与Inn谷地剪切带有关,并且与欧洲基底上的奥拓品单元的冲断有关。特伦托-维琴察地区的深地震活动与亚得里亚海下部地壳顶部的对齐证实了在南阿尔卑斯山发生深冲断层的建议。 (c)2005 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号