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Crust and upper mantle structure and its tectonic implications in the South China Sea and adjacent regions

机译:Crust and upper mantle structure and its tectonic implications in the south China sea and adjacent regions

摘要

We present a 3D S-velocity model for the crust and upper mantle of the South China Sea and the surrounding regions, constrained from the analysis of over 12,000 of fundamental Rayleigh wave dispersion curves between 10 s and 150 s periods. The lateral resolution was found to vary from degrees 2 to degrees 4 with the increasing period over the study region. A robust scheme of Debayle and Sambridge allowed us to conduct the tomographic inversion efficiently for massive datasets. Group velocity maps varying with period show lateral heterogeneities, well related to the geological and tectonic features in the study region. The 3D S-velocity model was constructed from the 1D structure inversion of the tomographic group velocity dispersion curves at each node. The obtained average crustal structure is similar to the PREM model, while the average mantle velocity is typically lower than the global average. The complicated 3D structures reveal three prominent features correlated with geological divisions: sea basin regions, island and arc regions, and continental regions. The derived crustal and lithospheric thicknesses range from similar to 15 to >50 km and from similar to 60 to >140 km, respectively, with the thinnest in the South China Sea, the thickest in eastern Tibet and the Yangtze Block, and the medium in the South China Fold Belt, Indochina, and island arc regions. Our results further confirm that (1) a Mesozoic subduction zone, which is interpreted as the tectonic weak zone during the Paleogene, exists along the South China margin; (2) the influence of the Indochina extrusion along the Red River Fault is limited for the South China Sea region; (3) there is a slab remnant of the proto-South China Sea beneath Borneo. New findings suggest that the Mesozoic subduction zone should be built into any evolution model for the region, as well as the other two major tectonic boundaries of the Red River Fault and proto-South China Sea subduction zone. (c) 2012 Elsevier Ltd. All rights reserved.
机译:我们通过分析10 s和150 s周期内超过12,000的基本瑞利波频散曲线,提出了南海及周边地区地壳和上地幔的3D S速度模型。发现横向分辨率随研究区域的增加而从2度到4度变化。 Debayle和Sambridge的健壮方案使我们能够对大量数据集进行高效的层析成像反演。随时间变化的群速度图显示出横向异质性,与研究区域的地质和构造特征密切相关。 3D S速度模型是根据每个节点的层析组速度色散曲线的1D结构反演而构建的。所获得的平均地壳结构类似于PREM模型,而平均地幔速度通常低于全局平均速度。复杂的3D结构揭示了与地质划分相关的三个突出特征:海盆区域,岛屿和弧形区域以及大陆区域。得出的地壳和岩石圈厚度分别从大约15 km至> 50 km和大约60 km至> 140 km,在南中国海最薄,在西藏东部和扬子地块最厚,而在华南褶皱带,印度支那和岛弧地区。我们的结果进一步证实:(1)中生代俯冲带,被解释为古近纪的构造弱带,位于华南边缘。 (2)南印度洋沿红河断裂的印度支那挤压作用有限。 (3)婆罗洲下面有一块原始南海遗迹。新发现表明,中生代俯冲带应建立在该地区的任何演化模型中,以及红河断裂带和南海原始俯冲带的其他两个主要构造边界内。 (c)2012 Elsevier Ltd.保留所有权利。

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