Crustal structure and extension mode in the northwestern margin of the South China Sea
Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin. These data constrain a hyper‐extended crustal area bounded by basin‐bounding faults corresponding to an aborted rift below the Xisha Trough w...
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| Published in | Geochemistry, geophysics, geosystems : G3 Vol. 17; no. 6; pp. 2143 - 2167 |
|---|---|
| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Washington
John Wiley & Sons, Inc
01.06.2016
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| Subjects | |
| Online Access | Get full text |
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| Abstract | Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin. These data constrain a hyper‐extended crustal area bounded by basin‐bounding faults corresponding to an aborted rift below the Xisha Trough with a subparallel fossil ridge in the adjacent Northwest Sub‐basin. The thinnest crust is located in the Xisha Trough, where it is remnant lower crust with a thickness of less than 3 km. Gravity modeling also revealed a hyper‐extended crust across the Xisha Trough. The postrift magmatism is well developed and more active in the Xisha Trough and farther southeast than on the northwestern continental margin of the South China Sea; and the magmatic intrusion/extrusion was relatively active during the rifting of Xisha Trough and the Northwest Sub‐basin. A narrow continent‐ocean transition zone with a width of ∼65 km bounded seaward by a volcanic buried seamount is characterized by crustal thinning, rift depression, low gravity anomaly and the termination of the break‐up unconformity seismic reflection. The aborted rift near the continental margin means that there may be no obvious detachment fault like that in the Iberia‐Newfoundland type margin. The symmetric rift, extreme hyper‐extended continental crust and hotter mantle materials indicate that continental crust underwent stretching phase (pure‐shear deformation), thinning phase and breakup followed by onset of seafloor spreading and the mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin.
Key Points
Multichannel seismic reflection and satellite gravity data in the northwestern South China Sea
Seismic images and gravity modeling indicate a hyper‐extended continental margin
Mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin |
|---|---|
| AbstractList | Combining multi-channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin. These data constrain a hyper-extended crustal area bounded by basin-bounding faults corresponding to an aborted rift below the Xisha Trough with a subparallel fossil ridge in the adjacent Northwest Sub-basin. The thinnest crust is located in the Xisha Trough, where it is remnant lower crust with a thickness of less than 3 km. Gravity modeling also revealed a hyper-extended crust across the Xisha Trough. The postrift magmatism is well developed and more active in the Xisha Trough and farther southeast than on the northwestern continental margin of the South China Sea; and the magmatic intrusion/extrusion was relatively active during the rifting of Xisha Trough and the Northwest Sub-basin. A narrow continent-ocean transition zone with a width of 65 km bounded seaward by a volcanic buried seamount is characterized by crustal thinning, rift depression, low gravity anomaly and the termination of the break-up unconformity seismic reflection. The aborted rift near the continental margin means that there may be no obvious detachment fault like that in the Iberia-Newfoundland type margin. The symmetric rift, extreme hyper-extended continental crust and hotter mantle materials indicate that continental crust underwent stretching phase (pure-shear deformation), thinning phase and breakup followed by onset of seafloor spreading and the mantle-lithosphere may break up before crustal-necking in the northwestern South China Sea margin. Key Points Multichannel seismic reflection and satellite gravity data in the northwestern South China Sea Seismic images and gravity modeling indicate a hyper-extended continental margin Mantle-lithosphere may break up before crustal-necking in the northwestern South China Sea margin Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin. These data constrain a hyper‐extended crustal area bounded by basin‐bounding faults corresponding to an aborted rift below the Xisha Trough with a subparallel fossil ridge in the adjacent Northwest Sub‐basin. The thinnest crust is located in the Xisha Trough, where it is remnant lower crust with a thickness of less than 3 km. Gravity modeling also revealed a hyper‐extended crust across the Xisha Trough. The postrift magmatism is well developed and more active in the Xisha Trough and farther southeast than on the northwestern continental margin of the South China Sea; and the magmatic intrusion/extrusion was relatively active during the rifting of Xisha Trough and the Northwest Sub‐basin. A narrow continent‐ocean transition zone with a width of ∼65 km bounded seaward by a volcanic buried seamount is characterized by crustal thinning, rift depression, low gravity anomaly and the termination of the break‐up unconformity seismic reflection. The aborted rift near the continental margin means that there may be no obvious detachment fault like that in the Iberia‐Newfoundland type margin. The symmetric rift, extreme hyper‐extended continental crust and hotter mantle materials indicate that continental crust underwent stretching phase (pure‐shear deformation), thinning phase and breakup followed by onset of seafloor spreading and the mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin. Key Points Multichannel seismic reflection and satellite gravity data in the northwestern South China Sea Seismic images and gravity modeling indicate a hyper‐extended continental margin Mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin Abstract Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin. These data constrain a hyper‐extended crustal area bounded by basin‐bounding faults corresponding to an aborted rift below the Xisha Trough with a subparallel fossil ridge in the adjacent Northwest Sub‐basin. The thinnest crust is located in the Xisha Trough, where it is remnant lower crust with a thickness of less than 3 km. Gravity modeling also revealed a hyper‐extended crust across the Xisha Trough. The postrift magmatism is well developed and more active in the Xisha Trough and farther southeast than on the northwestern continental margin of the South China Sea; and the magmatic intrusion/extrusion was relatively active during the rifting of Xisha Trough and the Northwest Sub‐basin. A narrow continent‐ocean transition zone with a width of ∼65 km bounded seaward by a volcanic buried seamount is characterized by crustal thinning, rift depression, low gravity anomaly and the termination of the break‐up unconformity seismic reflection. The aborted rift near the continental margin means that there may be no obvious detachment fault like that in the Iberia‐Newfoundland type margin. The symmetric rift, extreme hyper‐extended continental crust and hotter mantle materials indicate that continental crust underwent stretching phase (pure‐shear deformation), thinning phase and breakup followed by onset of seafloor spreading and the mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin. Key Points Multichannel seismic reflection and satellite gravity data in the northwestern South China Sea Seismic images and gravity modeling indicate a hyper‐extended continental margin Mantle‐lithosphere may break up before crustal‐necking in the northwestern South China Sea margin |
| Author | Mi, Lijun Spence, George McIntosh, Kirk Wu, Shiguo Liu, Zheng Gao, Jinwei |
| Author_xml | – sequence: 1 givenname: Jinwei surname: Gao fullname: Gao, Jinwei organization: Chinese Academy of Sciences – sequence: 2 givenname: Shiguo surname: Wu fullname: Wu, Shiguo organization: Qingdao National Laboratory for Marine Science and Technology – sequence: 3 givenname: Kirk surname: McIntosh fullname: McIntosh, Kirk organization: University of Texas at Austin (R2200) – sequence: 4 givenname: Lijun surname: Mi fullname: Mi, Lijun organization: China National Offshore Oil Corporation Ltd – sequence: 5 givenname: Zheng surname: Liu fullname: Liu, Zheng organization: China National Offshore Oil Corporation Ltd – sequence: 6 givenname: George surname: Spence fullname: Spence, George organization: University of Victoria |
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| Publisher | John Wiley & Sons, Inc |
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| Snippet | Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin.... Abstract Combining multi‐channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea... Combining multi-channel seismic reflection and gravity modeling, this study has investigated the crustal structure of the northwestern South China Sea margin.... |
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| SubjectTerms | Continental crust Continental margins crustal structure gravity modeling Lithosphere Magma multichannel seismic data Ocean floor Oceanography Plate tectonics Rifting rifting process Seafloor spreading Seamounts Seismology South China Sea Thinning Transition zone Unconformity Xisha Trough |
| Title | Crustal structure and extension mode in the northwestern margin of the South China Sea |
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