Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions
Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events record...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Xingchen [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Rechteinformationen: |
Nutzungsrecht: © Springer International Publishing 2016 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - [Basel] : Birkhäuser, 1964, 173(2016), 8, Seite 2727-2736 |
|---|---|
| Übergeordnetes Werk: |
volume:173 ; year:2016 ; number:8 ; pages:2727-2736 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00024-016-1293-0 |
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| 520 | |a Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. | ||
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10.1007/s00024-016-1293-0 doi PQ20160815 (DE-627)OLC1980109001 (DE-599)GBVOLC1980109001 (PRQ)springer_primary_2016_24_173_8_12930 (KEY)0066583520160000173000802727lithosphericstructureofthenortheasternnorthchinacr DE-627 ger DE-627 rakwb eng 550 DE-101 Wang, Xingchen verfasserin aut Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. Nutzungsrecht: © Springer International Publishing 2016 craton destruction Earth Sciences S receiver function Geophysics/Geodesy North China Craton lithospheric structure Ding, Zhifeng oth Zhu, Lupei oth Enthalten in Pure and applied geophysics [Basel] : Birkhäuser, 1964 173(2016), 8, Seite 2727-2736 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:173 year:2016 number:8 pages:2727-2736 http://dx.doi.org/10.1007/s00024-016-1293-0 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 AR 173 2016 8 2727-2736 |
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10.1007/s00024-016-1293-0 doi PQ20160815 (DE-627)OLC1980109001 (DE-599)GBVOLC1980109001 (PRQ)springer_primary_2016_24_173_8_12930 (KEY)0066583520160000173000802727lithosphericstructureofthenortheasternnorthchinacr DE-627 ger DE-627 rakwb eng 550 DE-101 Wang, Xingchen verfasserin aut Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. Nutzungsrecht: © Springer International Publishing 2016 craton destruction Earth Sciences S receiver function Geophysics/Geodesy North China Craton lithospheric structure Ding, Zhifeng oth Zhu, Lupei oth Enthalten in Pure and applied geophysics [Basel] : Birkhäuser, 1964 173(2016), 8, Seite 2727-2736 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:173 year:2016 number:8 pages:2727-2736 http://dx.doi.org/10.1007/s00024-016-1293-0 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 AR 173 2016 8 2727-2736 |
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10.1007/s00024-016-1293-0 doi PQ20160815 (DE-627)OLC1980109001 (DE-599)GBVOLC1980109001 (PRQ)springer_primary_2016_24_173_8_12930 (KEY)0066583520160000173000802727lithosphericstructureofthenortheasternnorthchinacr DE-627 ger DE-627 rakwb eng 550 DE-101 Wang, Xingchen verfasserin aut Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. Nutzungsrecht: © Springer International Publishing 2016 craton destruction Earth Sciences S receiver function Geophysics/Geodesy North China Craton lithospheric structure Ding, Zhifeng oth Zhu, Lupei oth Enthalten in Pure and applied geophysics [Basel] : Birkhäuser, 1964 173(2016), 8, Seite 2727-2736 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:173 year:2016 number:8 pages:2727-2736 http://dx.doi.org/10.1007/s00024-016-1293-0 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 AR 173 2016 8 2727-2736 |
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10.1007/s00024-016-1293-0 doi PQ20160815 (DE-627)OLC1980109001 (DE-599)GBVOLC1980109001 (PRQ)springer_primary_2016_24_173_8_12930 (KEY)0066583520160000173000802727lithosphericstructureofthenortheasternnorthchinacr DE-627 ger DE-627 rakwb eng 550 DE-101 Wang, Xingchen verfasserin aut Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. Nutzungsrecht: © Springer International Publishing 2016 craton destruction Earth Sciences S receiver function Geophysics/Geodesy North China Craton lithospheric structure Ding, Zhifeng oth Zhu, Lupei oth Enthalten in Pure and applied geophysics [Basel] : Birkhäuser, 1964 173(2016), 8, Seite 2727-2736 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:173 year:2016 number:8 pages:2727-2736 http://dx.doi.org/10.1007/s00024-016-1293-0 Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 AR 173 2016 8 2727-2736 |
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Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions |
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Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions |
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Wang, Xingchen |
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lithospheric structure of the northeastern north china craton imaged by s receiver functions |
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Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions |
| abstract |
Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. |
| abstractGer |
Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. |
| abstract_unstemmed |
Lithosphere thickness variation is important for understanding the significant tectonic reactivation of the North China Craton (NCC) in the Mesozoic and Cenozoic time. Here, we determined the lithospheric structure in the northeastern NCC using S receiver functions from 305 teleseismic events recorded by 223 seismic stations. The Moho and lithosphere–asthenosphere boundary (LAB) are imaged clearly beneath the region. The Moho depth decreases from ~45 km beneath the western NCC to ~25 km beneath the eastern NCC. We found that the lithospheric thickness varies from 60 to 80 km beneath the Trans-North China Orogen (TNCO) and eastern NCC with no significant change of the LAB depth. The lithosphere thickness beneath the northwestern Ordos plateau is 100–130 km. In addition, there is a mid-lithosphere discontinuity at a depth of 80 km beneath the plateau that is connected to the base of thinned lithosphere in TNCO and eastern NCC. We suggest that the mid-lithosphere discontinuity represents a mechanically weak zone in the original cratonic lithosphere of the NCC. The material in the lower lithosphere of the craton, when warmed and hydrated by water released from the subducting slab of Western Pacific, became weak due to decrease in viscosity and/or partial melting and was subsequently removed through small-scale mantle convections. |
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Lithospheric Structure of the Northeastern North China Craton Imaged by S Receiver Functions |
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