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2010年玉树7.1级地震震源区P和S波接收函数成像 被引量:10
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作者 沈旭章 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2013年第2期495-503,共9页
利用玉树固定地震台站和7个流动宽频带地震台站远震P波和S波接收函数,对2010年4月14日发生MS7.1级地震的玉树地震震源区下方地壳及上地幔顶部速度结构进行了成像.结果表明:研究区下方存在明显的双地壳结构;主震所在的金沙江缝合带可能... 利用玉树固定地震台站和7个流动宽频带地震台站远震P波和S波接收函数,对2010年4月14日发生MS7.1级地震的玉树地震震源区下方地壳及上地幔顶部速度结构进行了成像.结果表明:研究区下方存在明显的双地壳结构;主震所在的金沙江缝合带可能错断了地壳和岩石圈;错断的地壳在印度板块向北的推挤下,发生了叠置,导致金沙江缝合带下方呈现双地壳结构;根据发生在金沙江缝合带上的历史地震进一步推断,印度板块对金沙江缝合带这种深大走滑断裂的向北推挤,为断裂带上大地震的发生提供了闭锁条件,这可能是巴颜喀拉地块周边地震孕育的一种典型的深部地球动力学模式;在玉树地震主震区所在深度附近,发现局部存在高速夹层,这种局部高速结构,可能是积累引力,孕育地震的一个重要原因. 展开更多
关键词 玉树地震 P和S波接收函数成像 双地壳
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Bicharacteristic Curves in Modeling of the Earth Crust and Upper Mantle
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作者 Georgi Boyadzhiev 《Journal of Mathematics and System Science》 2014年第3期167-172,共6页
The aim of this paper is the introduction of a new approach to 3D modelling of elastic piecewise homogeneous media, in particular Earth crust and upper Mantle. The method is based on the principle of tomography with E... The aim of this paper is the introduction of a new approach to 3D modelling of elastic piecewise homogeneous media, in particular Earth crust and upper Mantle. The method is based on the principle of tomography with Earthquake as a source of the signal and receiver stations on the surface. The wave propagation in solid media is described by a system of three strongly coupled hyperbolic equations with piece - wise constant coefitients. The characteristic set and hi-characteristic curves of this system are computed in a homogeneous half-space with free boundary and the formulae of reflection and diffraction of the hi-characteristics on the internal boundaries of the media. Applications of the characteristic set and bi-eharacteristic curves for the inverse problem in geophysics and Earth modelling are given. 展开更多
关键词 3D modeling of Lithosphere BICHARACTERISTICS strongly coupled linear systems of PDE
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Late Triassic bivalves associated with a hydrothermal vent system in the Yidun Island Arc (SW China) of the eastern Tethys 被引量:2
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作者 LIN Li ZHU LiDong +4 位作者 PANG YanChun SHA JinGeng Franz T. FURSICH FU XiuGen WANG XinLi 《Science China Earth Sciences》 SCIE EI CAS 2011年第12期1864-1870,共7页
The Yidun Island Arc in the Three Rivers (Jinsha River, Lancang River, Nujiang River) region of southwestern China is one of the most important Kuroko-type volcanogenic massive sulfide deposits (VMS) in China. Intra-a... The Yidun Island Arc in the Three Rivers (Jinsha River, Lancang River, Nujiang River) region of southwestern China is one of the most important Kuroko-type volcanogenic massive sulfide deposits (VMS) in China. Intra-arc rifting of Yidun Island occurred during the Late Carnian-Norian when VMS deposits such as the Gacun Pb-Zn-Cu deposit were formed. A bivalve fauna was found in fine-grained tuffaceous slate and in mineralized tuffaceous siltstone containing very high contents of Pb (45.01-103.37 ppm) and Zn (135.78-300.03 ppm) of the upper Tumugou Formation in the Changtai-Gacun volcanic-sedimentary rift basin. Stratigraphically, the bivalve-bearing beds are equivalents of the Gacun Pb-Zn-Cu deposits. The diversity of this bivalve fauna is very low. It consists mainly of the thin-shelled, epibyssate suspension-feeding bivalves Pergamidia eumenea and Parapergamidia changtaiensis, the burrowing large, elongated, suspension-feeding Trigonodus keuperinus and Unionites? sp., and occasional specimens of the endobyssate suspension-feeding Trigonodus? sp. and the deep burrowing suspension-feeding Pleuromya markiamensis. Individuals of the first four taxa are so abundant that the specimens are sometimes concentrated in shell beds, probably indicating a gregarious habit. This bivalve fauna is associated with internal moulds of cylindrical, slightly conical tubes most likely produced by a worm-shaped organism. Composition, morphology, diversity, and high abundance of this fauna, chemical features of the surrounding sediment, and the tectonic setting all suggest that this bivalve fauna lived in a deep-water environment in or around a hydrothermal vent system. 展开更多
关键词 Late Triassic hydrothermal vents bivalves Yidun Island Arc of the eastern Tethys
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