Investigation of plateau basin crustal structures and thickening mechanisms in the northeastern margin of the Tibetan plateau
This paper uses deep seismic sounding (DSS) data to contrast and analyze the crustal structures of three plateau basins (Songpan-Garze, Qaidam, Longzhong) in the northeastern margin of the Qinghai-Xizang (Tibetan) plateau, as well as two stable cratonic basins (Ordos, Sichuan) in its peripheral area...
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Published in | Earthquake science Vol. 25; no. 5-6; pp. 385 - 397 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Beijing
Seismological Society of China
01.12.2012
Springer Nature B.V |
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Abstract | This paper uses deep seismic sounding (DSS) data to contrast and analyze the crustal structures of three plateau basins (Songpan-Garze, Qaidam, Longzhong) in the northeastern margin of the Qinghai-Xizang (Tibetan) plateau, as well as two stable cratonic basins (Ordos, Sichuan) in its peripheral areas. Plateau basin crustal structures, lithological variations and crustal thickening mechanisms were investigated. The results show that, compared to the peripheral stable cratonic basins, the crystalline crusts of plateau basins in the northeastern margin are up to 10–15 km thicker, and the relative medium velocity difference is about 5% less. The medium velocity change in crustal layers of plateau basin indicates that the upper crust undergoes brittle deformation, whereas the lower crust deforms plastically with low velocity. The middle crust shows a brittle-to-plastic transition zone in this region. Thickening in the lower crust (about 5–10 km), and rheological characteristics that show low-medium velocity (relatively reduced by 7%), suggest that crustal thickening mainly takes place in lower crust in the northeastern margin of the Tibetan plateau. The crust along the northeastern margin shows evidence of wholesale block movement, and crustal shortening and thickening seem to be the main deformation features of this region. The GPS data show that the block motion modes and crustal thickening in the Tibetan plateau is closely related to the peripheral tectonic stress field and motion direction of the Indian plate. The Mani-Yushu-Xianshuihe fold belt along the boundary between the Qiangtang block and the Bayan Har block divides the different plateau thickening tectonic environments into the middle-western plateau, the northeastern margin and the southeastern plateau. |
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AbstractList | This paper uses deep seismic sounding (DSS) data to contrast and analyze the crustal structures of three plateau basins (Songpan-Garze, Qaidam, Longzhong) in the northeastern margin of the Qinghai-Xizang (Tibetan) plateau, as well as two stable cratonic basins (Ordos, Sichuan) in its peripheral areas. Plateau basin crustal structures, lithological variations and crustal thickening mechanisms were investigated. The results show that, compared to the peripheral stable cratonic basins, the crystalline crusts of plateau basins in the northeastern margin are up to 10-15 km thicker, and the relative medium velocity difference is about 5% less. The medium velocity change in crustal layers of plateau basin indicates that the upper crust undergoes brittle deformation, whereas the lower crust deforms plastically with low velocity. The middle crust shows a brittle-to-plastic transition zone in this region. Thickening in the lower crust (about 5-10 km), and rheological characteristics that show low-medium velocity (relatively reduced by 7%), suggest that crustal thickening mainly takes place in lower crust in the northeastern margin of the Tibetan plateau. The crust along the northeastern margin shows evidence of wholesale block movement, and crustal shortening and thickening seem to be the main deformation features of this region. The GPS data show that the block motion modes and crustal thickening in the Tibetan plateau is closely related to the peripheral tectonic stress field and motion direction of the Indian plate. The Mani-Yushu-Xianshuihe fold belt along the boundary between the Qiangtang block and the Bayan Har block divides the different plateau thickening tectonic environments into the middle-western plateau, the northeastern margin and the southeastern plateau. This paper uses deep seismic sounding (DSS) data to contrast and analyze the crustal structures of three plateau basins (Songpan-Garze, Qaidam, Longzhong) in the northeastern margin of the Qinghai-Xizang (Tibetan) plateau, as well as two stable cratonic basins (Ordos, Sichuan) in its peripheral areas. Plateau basin crustal structures, lithological variations and crustal thickening mechanisms were investigated. The results show that, compared to the peripheral stable cratonic basins, the crystalline crusts of plateau basins in the northeastern margin are up to 10-15 km thicker, and the relative medium velocity difference is about 5% less. The medium velocity change in crustal layers of plateau basin indicates that the upper crust undergoes brittle deformation, whereas the lower crust deforms plastically with low velocity. The middle crust shows a brittle-to-plastic transition zone in this region. Thickening in the lower crust (about 5-10 km), and rheological characteristics that show low-medium velocity (relatively reduced by 7%), suggest that crustal thickening mainly takes place in lower crust in the northeastern margin of the Tibetan plateau. The crust along the northeastern margin shows evidence of wholesale block movement, and crustal shortening and thickening seem to be the main deformation features of this region. The GPS data show that the block motion modes and crustal thickening in the Tibetan plateau is closely related to the peripheral tectonic stress field and motion direction of the Indian plate. The Mani-Yushu-Xianshuihe fold belt along the boundary between the Qiangtang block and the Bayan Har block divides the different plateau thickening tectonic environments into the middle-western plateau, the northeastern margin and the southeastern plateau.[PUBLICATION ABSTRACT] |
Author | Lin, Jiyan Guo, Wenbin Liu, Zhi Jia, Shixu Zhang, Jianshi Xu, Zhaofan Liu, Baofeng |
Author_xml | – sequence: 1 givenname: Shixu surname: Jia fullname: Jia, Shixu email: jiasx111@sohu.com organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 2 givenname: Zhaofan surname: Xu fullname: Xu, Zhaofan organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 3 givenname: Zhi surname: Liu fullname: Liu, Zhi organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 4 givenname: Jianshi surname: Zhang fullname: Zhang, Jianshi organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 5 givenname: Baofeng surname: Liu fullname: Liu, Baofeng organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 6 givenname: Jiyan surname: Lin fullname: Lin, Jiyan organization: Geophysical Exploration Center, China Earthquake Administration – sequence: 7 givenname: Wenbin surname: Guo fullname: Guo, Wenbin organization: Geophysical Exploration Center, China Earthquake Administration |
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CitedBy_id | crossref_primary_10_1002_cjg2_30055 crossref_primary_10_1016_j_tecto_2023_229799 crossref_primary_10_1080_00206814_2021_1894610 crossref_primary_10_1016_j_tecto_2019_06_024 |
Cites_doi | 10.1007/s11430-009-0166-0 10.1046/j.0956-540x.2001.01402.x 10.1016/S0012-821X(03)00723-4 10.1038/366557a0 10.1146/annurev.earth.28.1.211 10.1029/2002JB001973 10.1126/science.274.5293.1684 10.1038/369642a0 10.1002/cjg2.1221 10.1016/0012-821X(96)00086-6 10.1016/j.jseaes.2010.03.010 10.1130/0091-7613(2000)28<703:TOBTEM>2.0.CO;2 10.1007/s11589-003-0028-3 10.1002/cjg2.1294 10.1126/science.1155371 10.1126/science.105978 10.1073/pnas.1001921107 10.1002/cjg2.233 10.1029/92JB00648 |
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Snippet | This paper uses deep seismic sounding (DSS) data to contrast and analyze the crustal structures of three plateau basins (Songpan-Garze, Qaidam, Longzhong) in... |
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SubjectTerms | Basins Blocking Boundaries Brittleness Crusts Deformation Earth and Environmental Science Earth Sciences Geophysics/Geodesy Tectonics Thickening Thickness measurement |
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Title | Investigation of plateau basin crustal structures and thickening mechanisms in the northeastern margin of the Tibetan plateau |
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