中亚和东南亚的弧形构造要素和上地幔结构:地震层析成像和地震数据

IF 1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
S. Yu. Sokolov, V. G. Trifonov
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引用次数: 0

摘要

摘要 对巽他弧内部上地幔羽流空间分布的分析表明,在巽他弧下沉板块从南面框定的停滞板块中,有许多羽流体。造成这种地幔结构的可能机制是:(i) W-E 向环状地幔流穿过平板坯的缝隙;(ii) 回滚能够在平板坯上形成缝隙,并在其中释放上地幔羽流,而没有深根(>1000 公里)。板顶上方的空间由局部热地幔体组成,这些热地幔体被认为是次级羽流,通常形成局部裂谷段。西藏和中亚地区速度变化 δVp 的三维可视化显示了与巽他弧地区类似的结构模式。我们可以观察到一个由亚水平板块碎片和缝隙组成的区域,该区域被深层和次生羽状异常所记录。从地震事件中探测到的沿巽他弧断层面的岩块运动矢量是从其曲率中心向外的,次生上地幔羽流集中于此。这表明弧前推力过程的发展与俯冲板块无关。伴随着弧形推力的是沿反向推力断层的少量位移。喜马拉雅山脉沿线的位移方位角呈扇形,朝向印度斯坦。这表明,构造活动(地震事件)的主要指标是从西藏境内的伸展型弧后盆地向南发生岩体位移的方向,并在沿剥离面运动的过程中产生了推力变形。喜马拉雅弧和巽他弧的地震运动有两个方向。第一个方向遵循印度板块俯冲模式。第二个方向包括沿推力平面向印度板块的可变方位角岩块运动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Arc Tectonic Elements and Upper Mantle Structure of Central and Southeast Asia: Seismic Tomography and Seismicity Data

Arc Tectonic Elements and Upper Mantle Structure of Central and Southeast Asia: Seismic Tomography and Seismicity Data

Abstract

Analysis of the upper mantle plumes spatial distribution in the inner part of the Sunda arc shows a number of plume bodies interrupting the stagnant slab framed from the south by the sinking slab of the Sunda arc. Possible mechanisms resulting in this structure of the mantle are (i) W-E-trending toroidal mantle flow through a gap in a flat slab and (ii) rollback capable of forming a gap in a flat slab and launching upper mantle plumes in it without deep (>1000 km) roots. The space above the top of the slab consists of local hot mantle bodies, which are considered secondary plumes and often form local rift segments. The 3D visualization of velocity variations δVp in the Tibet and Central Asia region demonstrates structural patterns similar to those in the Sunda arc area. One can observe a region of subhorizontal slab fragments and a gap, which is recorded by plume anomalies of deep and secondary origin. The motion vectors of the rock mass along the fault planes of the Sunda arc, detected from seismic events, are directed outward from its center of curvature, in which secondary upper mantle plumes are concentrated. This indicates the development of thrust processes at the arc front unassociated with the subducting plate. The arc thrusting is accompanied by a small number of displacements along antithetic thrust faults. The displacement azimuths along the Himalayas are fan-shaped, oriented toward Hindustan. This shows that the main indicator of tectonic activity (seismic events) has a direction of rock mass displacement to the south from the extensional back-arc basin within Tibet with the development of thrust deformations during movements along the detachment planes. Two directions of seismic movements are distinguished in the Himalayan arc, as well as in the Sunda arc. The first direction follows the Indian Plate subduction model. The second direction includes variable azimuth rock mass movements along the thrust planes onto the Indian Plate.

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来源期刊
Geotectonics
Geotectonics 地学-地球化学与地球物理
CiteScore
1.90
自引率
9.10%
发文量
28
审稿时长
3 months
期刊介绍: Geotectonics publishes articles on general and regional tectonics, structural geology, geodynamics, and experimental tectonics and considers the relation of tectonics to the deep structure of the earth, magmatism, metamorphism, and mineral resources.
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