Determination and Structural Analysis of the Lahijan Transverse Fault in Forestall Region of Alborz Mountains, Iran: A Geospatial Application

H. Safari, M. Ghasemi, R. R. Pash
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引用次数: 5

Abstract

The Lahijan fault zone (LFZ) is a transverse fault placed in a Forestall area of western Alborz Range, and cuts across this fold-thrust belt along the Sepid-rud valley. The results were later completed with field investigations. Analysis of the results of Geoinformatics Techniques (GiT) helped us to determine the limits and kinematics of the main fault zone and other related faults. The results showed that LFZ with N55E general strike, 90 km length and 30 km width extend from Sepid-rud dam to the Lahijan city. This fault zone, as a transversal fault, truncated and offset the western part of Alborz fold-thrust belt and thus, caused many structural complexities in this region. The results of structural investigations showed that LFZ was established as a leftlateral strike-slip fault zone. Several fault trends are generated by this tectonic regime.
伊朗Alborz山脉前缘Lahijan横断层的确定与构造分析:地理空间应用
拉希詹断裂带(Lahijan fault zone, LFZ)是位于Alborz山脉西部Forestall地区的横断断层,沿Sepid-rud山谷横断该褶皱冲断带。结果后来通过实地调查完成。对地理信息技术(GiT)结果的分析帮助我们确定了主断裂带和其他相关断层的界限和运动学。结果表明:从赛皮鲁德大坝到拉希让市,长90 km,宽30 km,具有N55E总走向。该断裂带作为一个横向断裂,截断和冲断了阿尔伯斯褶皱冲断带的西段,造成了该区构造的复杂性。构造调查结果表明,该区为左旋走滑断裂带。这一构造制度产生了若干断裂走向。
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