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Structural geometries and magnitude of shortening in the eastern Kura fold-thrust belt, Azerbaijan: Implications for the development of the Greater Caucasus Mountains

机译:阿塞拜疆东部库拉褶皱冲断带的结构几何形状和缩短的幅度:对大高加索山脉发展的影响

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The Greater Caucasus are the northernmost extent of the Arabia-Eurasia collision and are thought to represent the main locus of shortening within the central portion of the collision zone between 40° and 48°E. Recent work suggests that in detail, since the Plio-Pleistocene, much of the shortening in the eastern portion of the Caucasus system has been focused within the Kura fold-thrust belt along the southeastern margin of the Greater Caucasus. Here we present new field mapping and stratigraphic investigations of the eastern termination of the Kura fold-thrust belt in Azerbaijan to better constrain the structural geometries, magnitude of shortening, and initiation age for this portion of the fold-thrust belt. Our work suggests that this area of the fold-thrust belt exhibits significant along-strike variations in structural style and evolution and can effectively be divided into two distinct domains at ~48°E. The western domain is characterized by a subcritical median surface slope and isolated folds and thrusts propagating out of sequence, whereas the eastern domain is dominated by a single duplex structure and a history of in-sequence development in a critically tapered wedge. We hypothesize that these variations result from changes in relative rates of syn-tectonic sedimentation, erosion, and convergence velocity along strike. We find that within the western domain, the fold-thrust belt has accommodated ~12 km of total shortening. An unconformity within the western domain brackets the initiation age of this portion of the fold-thrust belt to between 1.8 and 0.88 Ma yielding permissible average shortening rates of between 6.7 and 13.6 mm/yr. Comparison of these average shortening rates to the geodetically measured shortening rate of 8 mm/yr indicates that since initiation, the fold-thrust belt has accommodated 83-100% of convergence between the Greater and Lesser Caucasus at this longitude.
机译:大高加索地区是阿拉伯-欧亚大陆碰撞的最北端,被认为是40°至48°E之间碰撞区中心部分内缩短的主要轨迹。最近的工作表明,自上新世以来,高加索体系东部的大部分缩短集中在大高加索东南边缘的库拉褶皱冲断带内。在这里,我们介绍了阿塞拜疆库拉褶皱冲断带东端的新的野外制图和地层学调查,以更好地限制褶皱冲断带这部分的结构几何形状,缩短的幅度和起始年龄。我们的工作表明,褶皱冲断带的这一区域在构造样式和演化过程中表现出明显的沿走动变化,并且可以在〜48°E有效地划分为两个不同的区域。西部域的特征是亚临界中值表面坡度和孤立的褶皱和逆冲传播的顺序,而东部域则由单双链体结构和临界楔形中的顺次发展史控制。我们假设这些变化是由于沿构造的构造沉积,侵蚀和收敛速度的相对速率的变化引起的。我们发现,在西部地区,褶皱冲断带已经适应了约12 km的总缩短。西部区域内的不整合将褶皱冲断带的这一部分的起始年龄括在1.8和0.88 Ma之间,产生的平均平均缩短率在6.7和13.6 mm / yr之间。将这些平均缩短率与大地测量的缩短率8 mm / yr进行比较,表明自开始以来,在该经度上,褶皱-冲断带已经适应了大高加索和小高加索之间的83-100%的收敛。

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  • 来源
    《Tectonics》 |2013年第3期|688-717|共30页
  • 作者单位

    Department of Geology, One Shields Avenue,University of California, Davis, CA 95616,USA;

    Department of Geology, University of California, Davis, California,USA;

    Geological Institute of Azerbaijan, Baku, Azerbaijan;

    Geological Institute of Azerbaijan, Baku, Azerbaijan;

    Faculty of Geology and Geophysics, University of Bucharest,Bucharest, Romania;

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