Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution
The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study w...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Shaoyi [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022transfer abstract |
|---|
| Übergeordnetes Werk: |
Enthalten in: Electrochemical synthesis of molybdenum sulfide semiconductor - Aliyev, Akif Shikhan ELSEVIER, 2015transfer abstract, international journal of applied and regional sedimentology, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:433 ; year:2022 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.sedgeo.2022.106133 |
|---|
| Katalog-ID: |
ELV057434484 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV057434484 | ||
| 003 | DE-627 | ||
| 005 | 20230626045115.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 220808s2022 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.sedgeo.2022.106133 |2 doi | |
| 028 | 5 | 2 | |a /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica |
| 035 | |a (DE-627)ELV057434484 | ||
| 035 | |a (ELSEVIER)S0037-0738(22)00054-9 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 530 |q VZ |
| 082 | 0 | 4 | |a 620 |q VZ |
| 082 | 0 | 4 | |a 690 |q VZ |
| 084 | |a 56.45 |2 bkl | ||
| 100 | 1 | |a Wang, Shaoyi |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| 264 | 1 | |c 2022transfer abstract | |
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. | ||
| 520 | |a The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. | ||
| 700 | 1 | |a Cheng, Yinhang |4 oth | |
| 700 | 1 | |a Jin, Ruoshi |4 oth | |
| 700 | 1 | |a Miao, Peisen |4 oth | |
| 700 | 1 | |a Zhang, Tianfu |4 oth | |
| 700 | 1 | |a Xu, Zenglian |4 oth | |
| 700 | 1 | |a Ao, Cong |4 oth | |
| 700 | 1 | |a Teng, Xueming |4 oth | |
| 700 | 1 | |a Cheng, Xianyu |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier |a Aliyev, Akif Shikhan ELSEVIER |t Electrochemical synthesis of molybdenum sulfide semiconductor |d 2015transfer abstract |d international journal of applied and regional sedimentology |g Amsterdam [u.a.] |w (DE-627)ELV018197035 |
| 773 | 1 | 8 | |g volume:433 |g year:2022 |g pages:0 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.sedgeo.2022.106133 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a GBV_ILN_40 | ||
| 936 | b | k | |a 56.45 |j Baustoffkunde |q VZ |
| 951 | |a AR | ||
| 952 | |d 433 |j 2022 |h 0 | ||
| author_variant |
s w sw |
|---|---|
| matchkey_str |
wangshaoyichengyinhangjinruoshimiaopeise:2022----:ertlicnpaeotertcostaanhsuhrsnlabsnehncnt |
| hierarchy_sort_str |
2022transfer abstract |
| bklnumber |
56.45 |
| publishDate |
2022 |
| allfields |
10.1016/j.sedgeo.2022.106133 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica (DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 DE-627 ger DE-627 rakwb eng 530 VZ 620 VZ 690 VZ 56.45 bkl Wang, Shaoyi verfasserin aut Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. Cheng, Yinhang oth Jin, Ruoshi oth Miao, Peisen oth Zhang, Tianfu oth Xu, Zenglian oth Ao, Cong oth Teng, Xueming oth Cheng, Xianyu oth Enthalten in Elsevier Aliyev, Akif Shikhan ELSEVIER Electrochemical synthesis of molybdenum sulfide semiconductor 2015transfer abstract international journal of applied and regional sedimentology Amsterdam [u.a.] (DE-627)ELV018197035 volume:433 year:2022 pages:0 https://doi.org/10.1016/j.sedgeo.2022.106133 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 56.45 Baustoffkunde VZ AR 433 2022 0 |
| spelling |
10.1016/j.sedgeo.2022.106133 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica (DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 DE-627 ger DE-627 rakwb eng 530 VZ 620 VZ 690 VZ 56.45 bkl Wang, Shaoyi verfasserin aut Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. Cheng, Yinhang oth Jin, Ruoshi oth Miao, Peisen oth Zhang, Tianfu oth Xu, Zenglian oth Ao, Cong oth Teng, Xueming oth Cheng, Xianyu oth Enthalten in Elsevier Aliyev, Akif Shikhan ELSEVIER Electrochemical synthesis of molybdenum sulfide semiconductor 2015transfer abstract international journal of applied and regional sedimentology Amsterdam [u.a.] (DE-627)ELV018197035 volume:433 year:2022 pages:0 https://doi.org/10.1016/j.sedgeo.2022.106133 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 56.45 Baustoffkunde VZ AR 433 2022 0 |
| allfields_unstemmed |
10.1016/j.sedgeo.2022.106133 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica (DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 DE-627 ger DE-627 rakwb eng 530 VZ 620 VZ 690 VZ 56.45 bkl Wang, Shaoyi verfasserin aut Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. Cheng, Yinhang oth Jin, Ruoshi oth Miao, Peisen oth Zhang, Tianfu oth Xu, Zenglian oth Ao, Cong oth Teng, Xueming oth Cheng, Xianyu oth Enthalten in Elsevier Aliyev, Akif Shikhan ELSEVIER Electrochemical synthesis of molybdenum sulfide semiconductor 2015transfer abstract international journal of applied and regional sedimentology Amsterdam [u.a.] (DE-627)ELV018197035 volume:433 year:2022 pages:0 https://doi.org/10.1016/j.sedgeo.2022.106133 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 56.45 Baustoffkunde VZ AR 433 2022 0 |
| allfieldsGer |
10.1016/j.sedgeo.2022.106133 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica (DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 DE-627 ger DE-627 rakwb eng 530 VZ 620 VZ 690 VZ 56.45 bkl Wang, Shaoyi verfasserin aut Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. Cheng, Yinhang oth Jin, Ruoshi oth Miao, Peisen oth Zhang, Tianfu oth Xu, Zenglian oth Ao, Cong oth Teng, Xueming oth Cheng, Xianyu oth Enthalten in Elsevier Aliyev, Akif Shikhan ELSEVIER Electrochemical synthesis of molybdenum sulfide semiconductor 2015transfer abstract international journal of applied and regional sedimentology Amsterdam [u.a.] (DE-627)ELV018197035 volume:433 year:2022 pages:0 https://doi.org/10.1016/j.sedgeo.2022.106133 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 56.45 Baustoffkunde VZ AR 433 2022 0 |
| allfieldsSound |
10.1016/j.sedgeo.2022.106133 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica (DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 DE-627 ger DE-627 rakwb eng 530 VZ 620 VZ 690 VZ 56.45 bkl Wang, Shaoyi verfasserin aut Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. Cheng, Yinhang oth Jin, Ruoshi oth Miao, Peisen oth Zhang, Tianfu oth Xu, Zenglian oth Ao, Cong oth Teng, Xueming oth Cheng, Xianyu oth Enthalten in Elsevier Aliyev, Akif Shikhan ELSEVIER Electrochemical synthesis of molybdenum sulfide semiconductor 2015transfer abstract international journal of applied and regional sedimentology Amsterdam [u.a.] (DE-627)ELV018197035 volume:433 year:2022 pages:0 https://doi.org/10.1016/j.sedgeo.2022.106133 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 56.45 Baustoffkunde VZ AR 433 2022 0 |
| language |
English |
| source |
Enthalten in Electrochemical synthesis of molybdenum sulfide semiconductor Amsterdam [u.a.] volume:433 year:2022 pages:0 |
| sourceStr |
Enthalten in Electrochemical synthesis of molybdenum sulfide semiconductor Amsterdam [u.a.] volume:433 year:2022 pages:0 |
| format_phy_str_mv |
Article |
| bklname |
Baustoffkunde |
| institution |
findex.gbv.de |
| dewey-raw |
530 |
| isfreeaccess_bool |
false |
| container_title |
Electrochemical synthesis of molybdenum sulfide semiconductor |
| authorswithroles_txt_mv |
Wang, Shaoyi @@aut@@ Cheng, Yinhang @@oth@@ Jin, Ruoshi @@oth@@ Miao, Peisen @@oth@@ Zhang, Tianfu @@oth@@ Xu, Zenglian @@oth@@ Ao, Cong @@oth@@ Teng, Xueming @@oth@@ Cheng, Xianyu @@oth@@ |
| publishDateDaySort_date |
2022-01-01T00:00:00Z |
| hierarchy_top_id |
ELV018197035 |
| dewey-sort |
3530 |
| id |
ELV057434484 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV057434484</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626045115.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220808s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.sedgeo.2022.106133</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV057434484</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0037-0738(22)00054-9</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">530</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">56.45</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wang, Shaoyi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cheng, Yinhang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jin, Ruoshi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Miao, Peisen</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Tianfu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Zenglian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ao, Cong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Teng, Xueming</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cheng, Xianyu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Aliyev, Akif Shikhan ELSEVIER</subfield><subfield code="t">Electrochemical synthesis of molybdenum sulfide semiconductor</subfield><subfield code="d">2015transfer abstract</subfield><subfield code="d">international journal of applied and regional sedimentology</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV018197035</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:433</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.sedgeo.2022.106133</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">56.45</subfield><subfield code="j">Baustoffkunde</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">433</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| author |
Wang, Shaoyi |
| spellingShingle |
Wang, Shaoyi ddc 530 ddc 620 ddc 690 bkl 56.45 Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| authorStr |
Wang, Shaoyi |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV018197035 |
| format |
electronic Article |
| dewey-ones |
530 - Physics 620 - Engineering & allied operations 690 - Buildings |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
530 VZ 620 VZ 690 VZ 56.45 bkl Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| topic |
ddc 530 ddc 620 ddc 690 bkl 56.45 |
| topic_unstemmed |
ddc 530 ddc 620 ddc 690 bkl 56.45 |
| topic_browse |
ddc 530 ddc 620 ddc 690 bkl 56.45 |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
y c yc r j rj p m pm t z tz z x zx c a ca x t xt x c xc |
| hierarchy_parent_title |
Electrochemical synthesis of molybdenum sulfide semiconductor |
| hierarchy_parent_id |
ELV018197035 |
| dewey-tens |
530 - Physics 620 - Engineering 690 - Building & construction |
| hierarchy_top_title |
Electrochemical synthesis of molybdenum sulfide semiconductor |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV018197035 |
| title |
Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| ctrlnum |
(DE-627)ELV057434484 (ELSEVIER)S0037-0738(22)00054-9 |
| title_full |
Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| author_sort |
Wang, Shaoyi |
| journal |
Electrochemical synthesis of molybdenum sulfide semiconductor |
| journalStr |
Electrochemical synthesis of molybdenum sulfide semiconductor |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science 600 - Technology |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Wang, Shaoyi |
| container_volume |
433 |
| class |
530 VZ 620 VZ 690 VZ 56.45 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Wang, Shaoyi |
| doi_str_mv |
10.1016/j.sedgeo.2022.106133 |
| dewey-full |
530 620 690 |
| title_sort |
detrital zircon u-pb ages of the cretaceous strata in the southern songliao basin, ne china: constraints on basin-and-range evolution |
| title_auth |
Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| abstract |
The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. |
| abstractGer |
The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. |
| abstract_unstemmed |
The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_40 |
| title_short |
Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution |
| url |
https://doi.org/10.1016/j.sedgeo.2022.106133 |
| remote_bool |
true |
| author2 |
Cheng, Yinhang Jin, Ruoshi Miao, Peisen Zhang, Tianfu Xu, Zenglian Ao, Cong Teng, Xueming Cheng, Xianyu |
| author2Str |
Cheng, Yinhang Jin, Ruoshi Miao, Peisen Zhang, Tianfu Xu, Zenglian Ao, Cong Teng, Xueming Cheng, Xianyu |
| ppnlink |
ELV018197035 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth oth oth oth oth |
| doi_str |
10.1016/j.sedgeo.2022.106133 |
| up_date |
2024-07-06T23:13:21.854Z |
| _version_ |
1803873263922708480 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV057434484</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626045115.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220808s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.sedgeo.2022.106133</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001763.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV057434484</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0037-0738(22)00054-9</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">530</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">620</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">56.45</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wang, Shaoyi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Detrital zircon U-Pb ages of the Cretaceous strata in the southern Songliao Basin, NE China: Constraints on basin-and-range evolution</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The basin-and-range evolution of Northeast China could provide a comprehensive understanding of the subduction of the Paleo-Pacific Plate. The Songliao Basin preserved the essential and complete records of the Cretaceous tectonic evolution. The systematic detrital zircon UPb geochronological study was conducted on the Cretaceous sequences in the southern Songliao Basin, including Yingcheng Formation, Denglouku Formation, Quantou Formation, Qingshankou Formation, Yaojia Formation, Nenjiang Formation from bottom to up, providing new insights of provenances and tectonic evolution of the basin-range system. The Aptian and Albian sequences with the dominant age populations at ca. 133–125 Ma were derived from the Great Xing'an Range (GXAR). The Cenomanian and Early Turonian sequences with the distinct age populations at ca. 243–227 Ma received the source from the southernmost part of the Zhangguangcai Range (ZGCR). The Late Turonian to Campanian sequences experienced the gradual provenance transition to the GXAR. The main interim period with the dominant peaks at ca.1.8 and 2.5 Ga, and subdominant peaks at ca. 277 Ma, reveals the provenances from the southern margin, including the Inner Mongolia Paleo-Uplift (IMPU) and northern North China craton (NNCC) during the Late Turonian to Early Santonian. Since then, the provenance was skewed towards the GXAR manifesting the distinct age populations at ca. 139 Ma. The multi-provenance transitions reveal two orogeneses of the GXAR and ZGCR with the difference of 9 Ma. The gradual uplift from north to south in the Jiamusi Massif and the ZGCR at ca. 120–90 Ma was related to magmatic activity under the transition from the low angle subduction to slab rollback of the Pacific-Plate. The integral uplift of the GXAR at ca. 90–83.8 Ma was related to the transient compression due to the changes in direction and convergence rate of the Paleo-Pacific Plate. The compression-induced uplift was more intense than magmatism-induced uplift. Our findings can contribute to a better understanding of the basin-and-range evolution of Northeast China and the response to the subduction of the Paleo-Pacific Plate.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cheng, Yinhang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jin, Ruoshi</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Miao, Peisen</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhang, Tianfu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Zenglian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ao, Cong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Teng, Xueming</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cheng, Xianyu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Aliyev, Akif Shikhan ELSEVIER</subfield><subfield code="t">Electrochemical synthesis of molybdenum sulfide semiconductor</subfield><subfield code="d">2015transfer abstract</subfield><subfield code="d">international journal of applied and regional sedimentology</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV018197035</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:433</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.sedgeo.2022.106133</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">56.45</subfield><subfield code="j">Baustoffkunde</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">433</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.398695 |