The newly recognized ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton: Petrogenesis and tectonic implications
• Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline r...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kong, Ling-Hao [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study - Salunkhe, R. ELSEVIER, 2017, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:383 ; year:2022 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1016/j.precamres.2022.106904 |
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| 520 | |a • Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. | ||
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10.1016/j.precamres.2022.106904 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001983.pica (DE-627)ELV059764937 (ELSEVIER)S0301-9268(22)00348-5 DE-627 ger DE-627 rakwb eng 610 VZ 570 540 VZ Kong, Ling-Hao verfasserin aut The newly recognized ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton: Petrogenesis and tectonic implications 2022 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. North China Craton (NCC) Elsevier Geochronology Elsevier Paleogeographic reconstruction Elsevier Dolerite sills Elsevier Continental flood basalt Elsevier Large igneous province (LIP) Elsevier Zhang, Shuan-Hong oth Hu, Guo-Hui oth Wang, Hong-Yu oth Cai, Yu-Hang oth Pei, Jun-Ling oth Zhang, Qi-Qi oth Zhao, Yue oth Enthalten in Elsevier Science Salunkhe, R. ELSEVIER OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study 2017 Amsterdam [u.a.] (DE-627)ELV014866900 volume:383 year:2022 pages:0 https://doi.org/10.1016/j.precamres.2022.106904 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 AR 383 2022 0 |
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10.1016/j.precamres.2022.106904 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001983.pica (DE-627)ELV059764937 (ELSEVIER)S0301-9268(22)00348-5 DE-627 ger DE-627 rakwb eng 610 VZ 570 540 VZ Kong, Ling-Hao verfasserin aut The newly recognized ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton: Petrogenesis and tectonic implications 2022 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. North China Craton (NCC) Elsevier Geochronology Elsevier Paleogeographic reconstruction Elsevier Dolerite sills Elsevier Continental flood basalt Elsevier Large igneous province (LIP) Elsevier Zhang, Shuan-Hong oth Hu, Guo-Hui oth Wang, Hong-Yu oth Cai, Yu-Hang oth Pei, Jun-Ling oth Zhang, Qi-Qi oth Zhao, Yue oth Enthalten in Elsevier Science Salunkhe, R. ELSEVIER OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study 2017 Amsterdam [u.a.] (DE-627)ELV014866900 volume:383 year:2022 pages:0 https://doi.org/10.1016/j.precamres.2022.106904 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 AR 383 2022 0 |
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newly recognized ca. 1.23–1.21 ga dolerite sills and flood basalts from fanhe basin in the northeastern north china craton: petrogenesis and tectonic implications |
| title_auth |
The newly recognized ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton: Petrogenesis and tectonic implications |
| abstract |
• Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. |
| abstractGer |
• Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. |
| abstract_unstemmed |
• Identification of the ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton. • The ca. 1.23–1.21 Ga mafic rocks can be divided into alkaline and sub-alkaline series and exhibit distinct trace element and Nd isotopic compositions. • The alkaline rocks were derived from an OIB-like asthenospheric mantle source. • The sub-alkaline rocks were derived from a subduction-modified subcontinental lithospheric mantle. |
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GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 |
| title_short |
The newly recognized ca. 1.23–1.21 Ga dolerite sills and flood basalts from Fanhe Basin in the northeastern North China Craton: Petrogenesis and tectonic implications |
| url |
https://doi.org/10.1016/j.precamres.2022.106904 |
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| author2 |
Zhang, Shuan-Hong Hu, Guo-Hui Wang, Hong-Yu Cai, Yu-Hang Pei, Jun-Ling Zhang, Qi-Qi Zhao, Yue |
| author2Str |
Zhang, Shuan-Hong Hu, Guo-Hui Wang, Hong-Yu Cai, Yu-Hang Pei, Jun-Ling Zhang, Qi-Qi Zhao, Yue |
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| doi_str |
10.1016/j.precamres.2022.106904 |
| up_date |
2024-07-06T22:59:22.296Z |
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1803872383582339072 |
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