Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea
Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of sei...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Xie, Xinong [verfasserIn] Ren, Jianye [verfasserIn] Pang, Xiong [verfasserIn] Lei, Chao [verfasserIn] Chen, Hui [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Marine geophysical research - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970, 40(2019), 2 vom: 29. Jan., Seite 129-144 |
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| Übergeordnetes Werk: |
volume:40 ; year:2019 ; number:2 ; day:29 ; month:01 ; pages:129-144 |
| Links: |
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| DOI / URN: |
10.1007/s11001-019-09378-6 |
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SPR015479633 |
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| 520 | |a Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. | ||
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10.1007/s11001-019-09378-6 doi (DE-627)SPR015479633 (SPR)s11001-019-09378-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.70 bkl 38.90 bkl Xie, Xinong verfasserin aut Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 Ren, Jianye verfasserin aut Pang, Xiong verfasserin aut Lei, Chao verfasserin aut Chen, Hui verfasserin aut Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 40(2019), 2 vom: 29. Jan., Seite 129-144 (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:40 year:2019 number:2 day:29 month:01 pages:129-144 https://dx.doi.org/10.1007/s11001-019-09378-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.70 ASE 38.90 ASE AR 40 2019 2 29 01 129-144 |
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10.1007/s11001-019-09378-6 doi (DE-627)SPR015479633 (SPR)s11001-019-09378-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.70 bkl 38.90 bkl Xie, Xinong verfasserin aut Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 Ren, Jianye verfasserin aut Pang, Xiong verfasserin aut Lei, Chao verfasserin aut Chen, Hui verfasserin aut Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 40(2019), 2 vom: 29. Jan., Seite 129-144 (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:40 year:2019 number:2 day:29 month:01 pages:129-144 https://dx.doi.org/10.1007/s11001-019-09378-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.70 ASE 38.90 ASE AR 40 2019 2 29 01 129-144 |
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10.1007/s11001-019-09378-6 doi (DE-627)SPR015479633 (SPR)s11001-019-09378-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.70 bkl 38.90 bkl Xie, Xinong verfasserin aut Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 Ren, Jianye verfasserin aut Pang, Xiong verfasserin aut Lei, Chao verfasserin aut Chen, Hui verfasserin aut Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 40(2019), 2 vom: 29. Jan., Seite 129-144 (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:40 year:2019 number:2 day:29 month:01 pages:129-144 https://dx.doi.org/10.1007/s11001-019-09378-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.70 ASE 38.90 ASE AR 40 2019 2 29 01 129-144 |
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10.1007/s11001-019-09378-6 doi (DE-627)SPR015479633 (SPR)s11001-019-09378-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.70 bkl 38.90 bkl Xie, Xinong verfasserin aut Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 Ren, Jianye verfasserin aut Pang, Xiong verfasserin aut Lei, Chao verfasserin aut Chen, Hui verfasserin aut Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 40(2019), 2 vom: 29. Jan., Seite 129-144 (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:40 year:2019 number:2 day:29 month:01 pages:129-144 https://dx.doi.org/10.1007/s11001-019-09378-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.70 ASE 38.90 ASE AR 40 2019 2 29 01 129-144 |
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10.1007/s11001-019-09378-6 doi (DE-627)SPR015479633 (SPR)s11001-019-09378-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.70 bkl 38.90 bkl Xie, Xinong verfasserin aut Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 Ren, Jianye verfasserin aut Pang, Xiong verfasserin aut Lei, Chao verfasserin aut Chen, Hui verfasserin aut Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 40(2019), 2 vom: 29. Jan., Seite 129-144 (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:40 year:2019 number:2 day:29 month:01 pages:129-144 https://dx.doi.org/10.1007/s11001-019-09378-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.70 ASE 38.90 ASE AR 40 2019 2 29 01 129-144 |
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Enthalten in Marine geophysical research 40(2019), 2 vom: 29. Jan., Seite 129-144 volume:40 year:2019 number:2 day:29 month:01 pages:129-144 |
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Enthalten in Marine geophysical research 40(2019), 2 vom: 29. Jan., Seite 129-144 volume:40 year:2019 number:2 day:29 month:01 pages:129-144 |
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Stratigraphic architecture Seafloor spreading of South China Sea Passive continental margin Pearl River Mouth basin |
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Xie, Xinong @@aut@@ Ren, Jianye @@aut@@ Pang, Xiong @@aut@@ Lei, Chao @@aut@@ Chen, Hui @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR015479633</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111022001.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11001-019-09378-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR015479633</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11001-019-09378-6-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.70</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.90</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Xie, Xinong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. 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Xie, Xinong |
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Xie, Xinong ddc 550 bkl 38.70 bkl 38.90 misc Stratigraphic architecture misc Seafloor spreading of South China Sea misc Passive continental margin misc Pearl River Mouth basin Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea |
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550 ASE 38.70 bkl 38.90 bkl Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea Stratigraphic architecture (dpeaa)DE-He213 Seafloor spreading of South China Sea (dpeaa)DE-He213 Passive continental margin (dpeaa)DE-He213 Pearl River Mouth basin (dpeaa)DE-He213 |
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ddc 550 bkl 38.70 bkl 38.90 misc Stratigraphic architecture misc Seafloor spreading of South China Sea misc Passive continental margin misc Pearl River Mouth basin |
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Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea |
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stratigraphic architectures and associated unconformities of pearl river mouth basin during rifting and lithospheric breakup of the south china sea |
| title_auth |
Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea |
| abstract |
Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. |
| abstractGer |
Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. |
| abstract_unstemmed |
Abstract The lithosphere breakup processes from initial rifting of the crust to the complete rupture of the lithosphere underwent several tectonic evolution stages and resulted in the formation of a distinct stratigraphic architecture and associated unconformities. In this study, a dense grid of seismic profiles tied to industrial borehole data are used to investigate the stratigraphic architecture and unconformity interfaces in the Pearl River Mouth basin of the northern South China Sea margin. The Pearl River Mouth typed rifted margin evolved from stretching, thinning, to finally seafloor spreading. Our results indicate that a distinct stratigraphic architecture with well defined unconformities are formed in the proximal to distal zone of the margin. The syn-rift strata have been constrained by the top of basement unconformity and the lithosphere breakup unconformity. Polyphase rift strata during lithospheric rupture process are mainly controlled by two fault patterns, high-angle normal faults and low-angle detachment faults. In the proximal domain, multiple episodes of syn-rift strata are characterized by vertical superimposed half-graben or graben type stratigraphic patterns separated by crack-related unconformity. However, in the more distal zones, syn-rift strata composed two distinct intervals separated by detachment-related unconformity, including small-scaled dispersed half-graben or graben at the lower part and large-scaled wide syn-detachment depression at the upper part. Based on these observations we provide an effective method for the correlation of sedimentary strata from the proximal to distal domains of the passive rifted margins during the lithospheric rupture process. |
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Stratigraphic architectures and associated unconformities of Pearl River Mouth basin during rifting and lithospheric breakup of the South China Sea |
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Ren, Jianye Pang, Xiong Lei, Chao Chen, Hui |
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2024-07-03T16:31:27.315Z |
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| score |
7.402094 |