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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Insights from scaled analogue modelling into the seismotectonics of the Iranian region
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Insights from scaled analogue modelling into the seismotectonics of the Iranian region

机译:从比例模拟模型到伊朗地区地震构造的见解

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摘要

We show how analogue modelling provides insights into complex crustal block kinematics and the seismotectonics of active areas undergoing contraction, such as the Iranian region. The seismotectonic model deriving from this analysis is consistent with partitioning of the N-directed Arabia indentation into a composite system of collision-oblique and collision-parallel seismogenetic belts. These features include (1) two main conjugate transpressive belts (the dextral NW-SE-trending Zagros belt and the NE-SW-trending sinistral Elburz-Aran-Torud (EAT) belt), and (2) a modest lateral escape of Central Iran towards the Lut block along the Nayband belt. This cinematic model fits the seismic activity and the current fault pattern of the region. Also, the velocity field scaled from the model to nature shows a good similarity with previous numerical modelling as well as with deformation rates along the first-order seismogenetic belts determined by plate tectonic models and GPS data. (C) 2003 Elsevier B.V. All rights reserved. [References: 46]
机译:我们展示了模拟建模如何为复杂的地壳运动学和活动区域(如伊朗地区)的地震构造提供了见识。从该分析得出的地震构造模型与将N向阿拉伯压痕划分为碰撞倾斜和碰撞平行地震成因带的复合系统相一致。这些特征包括:(1)两个主要的共轭超压带(右旋NW-SE趋势Zagros带和NE-SW趋势左弦Elburz-Aran-Torud(EAT)带),以及(2)中央的适度侧向逃逸伊朗沿着内班德带向卢特街区行驶。该电影模型适合该地区的地震活动和当前断层模式。此外,从模型到自然尺度的速度场与以前的数值模型以及由板块构造模型和GPS数据确定的沿一阶地震发生带的变形率显示出良好的相似性。 (C)2003 Elsevier B.V.保留所有权利。 [参考:46]

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