基于三重震相的青藏高原东缘岩石圈地幔波速结构 |
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引用本文: | 眭怡,吴庆举,张瑞青. 基于三重震相的青藏高原东缘岩石圈地幔波速结构[J]. 地震学报, 2018, 40(5): 537-546. DOI: 10.11939/jass.20180030 |
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作者姓名: | 眭怡 吴庆举 张瑞青 |
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作者单位: | 1.中国北京 100081 中国地震局地球物理研究所 |
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基金项目: | 中国地震局地球研究所基本科研业务费专项(DQJB16B09)、国家自然科学基金青年基金项目(41604073)和国家自然科学基金面上项目(41474089)共同资助 |
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摘 要: | 本文利用中国数字地震台网记录到的中国青海和缅甸弧发生的两次浅源地震的区域波形资料,在以Crust2.0改进AK135模型所构建的参考模型C2AK的基础上,通过三重震相波形拟合的方法,获得了青藏高原东部下方从莫霍面至上地幔顶部180 km深度范围内的P波和S波最佳拟合模型。最佳模型显示:松潘—甘孜地块(A和B剖面)下方的P波速度比C2AK模型高5%,而川滇地块(C剖面)下方上地幔顶部的P波速度要比参考模型低5%,且随深度逐渐增加,直至120 km处与C2AK模型值相同;松潘—甘孜地块下方的S波速度较C2AK模型要高3%。上述区域性速度结构差异表明,相对于松潘—甘孜地块,川滇地区的岩石圈地幔存在着更明显的挤出效应。
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关 键 词: | 青藏东缘 岩石圈 地震三重震相 速度结构 |
收稿时间: | 2018-03-05 |
Lithospheric velocity structure of eastern Tibet Plateau from triplication |
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Affiliation: | 1.Institute of Geophysics,China Earthquake Administration,Beijing 100081,China2.Key Laboratory of Seismic Observation and Geophysical Imaging,Beijing 100081,China |
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Abstract: | By comparing the synthetic and observed seismic triplications for two events from Qinghai and Myanmar Arc with the trial-and-error method, the velocity structures of P-wave and S-wave from Moho to the depth of 180 km are obtained. The P-wave velocity models for the profiles A and B beneath Songpan-Garze block are 5% higher than that in the model C2AK, which is based on the model AK135 with crust structure of Crust2.0. The P-wave velocity model for the profile C beneath Sichuan-Yunnan block, however, is 5% lower than that in the model C2AK at Moho depth, and then increases slowly down to the depth of 120 km. The S-wave velocity model beneath Songpan-Garze block is 3% higher than the model C2AK from Moho to 180 km. Such regional difference in velocity structure may indicate that the lithospheric mantle beneath Sichuan-Yunnan block has been extruded more obviously than that beneath Songpan-Garze block in the uplift of the Tibetan Plateau. |
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