Sedimentology of a topset-dominated, braided river delta of Huangqihai Lake, North China: implications for formation mechanisms
Abstract Sedimentary characteristics and genesis of a sandy, topset-dominated braided river delta from Huangqihai Lake were investigated using trenching and a ground penetrating radar survey. Ten lithofacies types were identified with assistance of grain size distribution to record a broad range of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Shan, Xin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media Dordrecht 2016 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of paleolimnology - Springer Netherlands, 1988, 59(2016), 2 vom: 14. Nov., Seite 245-261 |
|---|---|
| Übergeordnetes Werk: |
volume:59 ; year:2016 ; number:2 ; day:14 ; month:11 ; pages:245-261 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10933-016-9929-8 |
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OLC2071095987 |
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| 520 | |a Abstract Sedimentary characteristics and genesis of a sandy, topset-dominated braided river delta from Huangqihai Lake were investigated using trenching and a ground penetrating radar survey. Ten lithofacies types were identified with assistance of grain size distribution to record a broad range of depositional processes within an overall coarsening upward sequence. Four distinct architectural elements, including channel fill, compound bar, sand sheet, and river mouth bar, built up this delta. No obvious foreset can be identified in this braided river delta. A gentle slope (0.2°) and shallow basin (<10 m deep), young age (~25 years), and low sediment supply caused by human disturbance and semi-arid climate, are believed to allow this type of topset-dominated delta to form. | ||
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570 930 |
| title_sort |
sedimentology of a topset-dominated, braided river delta of huangqihai lake, north china: implications for formation mechanisms |
| title_auth |
Sedimentology of a topset-dominated, braided river delta of Huangqihai Lake, North China: implications for formation mechanisms |
| abstract |
Abstract Sedimentary characteristics and genesis of a sandy, topset-dominated braided river delta from Huangqihai Lake were investigated using trenching and a ground penetrating radar survey. Ten lithofacies types were identified with assistance of grain size distribution to record a broad range of depositional processes within an overall coarsening upward sequence. Four distinct architectural elements, including channel fill, compound bar, sand sheet, and river mouth bar, built up this delta. No obvious foreset can be identified in this braided river delta. A gentle slope (0.2°) and shallow basin (<10 m deep), young age (~25 years), and low sediment supply caused by human disturbance and semi-arid climate, are believed to allow this type of topset-dominated delta to form. © Springer Science+Business Media Dordrecht 2016 |
| abstractGer |
Abstract Sedimentary characteristics and genesis of a sandy, topset-dominated braided river delta from Huangqihai Lake were investigated using trenching and a ground penetrating radar survey. Ten lithofacies types were identified with assistance of grain size distribution to record a broad range of depositional processes within an overall coarsening upward sequence. Four distinct architectural elements, including channel fill, compound bar, sand sheet, and river mouth bar, built up this delta. No obvious foreset can be identified in this braided river delta. A gentle slope (0.2°) and shallow basin (<10 m deep), young age (~25 years), and low sediment supply caused by human disturbance and semi-arid climate, are believed to allow this type of topset-dominated delta to form. © Springer Science+Business Media Dordrecht 2016 |
| abstract_unstemmed |
Abstract Sedimentary characteristics and genesis of a sandy, topset-dominated braided river delta from Huangqihai Lake were investigated using trenching and a ground penetrating radar survey. Ten lithofacies types were identified with assistance of grain size distribution to record a broad range of depositional processes within an overall coarsening upward sequence. Four distinct architectural elements, including channel fill, compound bar, sand sheet, and river mouth bar, built up this delta. No obvious foreset can be identified in this braided river delta. A gentle slope (0.2°) and shallow basin (<10 m deep), young age (~25 years), and low sediment supply caused by human disturbance and semi-arid climate, are believed to allow this type of topset-dominated delta to form. © Springer Science+Business Media Dordrecht 2016 |
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| container_issue |
2 |
| title_short |
Sedimentology of a topset-dominated, braided river delta of Huangqihai Lake, North China: implications for formation mechanisms |
| url |
https://doi.org/10.1007/s10933-016-9929-8 |
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| author2 |
Li, Shengli Li, Shunli Yu, Xinghe Wan, Li Jin, Lina Wang, Tianyi |
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Li, Shengli Li, Shunli Yu, Xinghe Wan, Li Jin, Lina Wang, Tianyi |
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| doi_str |
10.1007/s10933-016-9929-8 |
| up_date |
2024-07-04T02:56:25.304Z |
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