Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province
Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial adva...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wei, Zhang [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Anmerkung: |
© Springer 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of geographical sciences - Science in China Press, 2001, 15(2005), 4 vom: Okt., Seite 448-458 |
|---|---|
| Übergeordnetes Werk: |
volume:15 ; year:2005 ; number:4 ; month:10 ; pages:448-458 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02892152 |
|---|
| Katalog-ID: |
OLC2051256640 |
|---|
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| 520 | |a Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. | ||
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| 700 | 1 | |a Jianqiang, Yang |4 aut | |
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10.1007/BF02892152 doi (DE-627)OLC2051256640 (DE-He213)BF02892152-p DE-627 ger DE-627 rakwb eng 910 VZ 14 ssgn 74.00$jGeographie$jAnthropogeographie: Allgemeines bkl Wei, Zhang verfasserin aut Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer 2005 Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. Zhijiu, Cui aut Jinliang, Feng aut Chaolu, Yi aut Jianqiang, Yang aut Enthalten in Journal of geographical sciences Science in China Press, 2001 15(2005), 4 vom: Okt., Seite 448-458 (DE-627)33352800X (DE-600)2055945-8 (DE-576)094642230 1009-637X nnns volume:15 year:2005 number:4 month:10 pages:448-458 https://doi.org/10.1007/BF02892152 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_4314 74.00$jGeographie$jAnthropogeographie: Allgemeines VZ 106417150 (DE-625)106417150 AR 15 2005 4 10 448-458 |
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10.1007/BF02892152 doi (DE-627)OLC2051256640 (DE-He213)BF02892152-p DE-627 ger DE-627 rakwb eng 910 VZ 14 ssgn 74.00$jGeographie$jAnthropogeographie: Allgemeines bkl Wei, Zhang verfasserin aut Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer 2005 Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. Zhijiu, Cui aut Jinliang, Feng aut Chaolu, Yi aut Jianqiang, Yang aut Enthalten in Journal of geographical sciences Science in China Press, 2001 15(2005), 4 vom: Okt., Seite 448-458 (DE-627)33352800X (DE-600)2055945-8 (DE-576)094642230 1009-637X nnns volume:15 year:2005 number:4 month:10 pages:448-458 https://doi.org/10.1007/BF02892152 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_4314 74.00$jGeographie$jAnthropogeographie: Allgemeines VZ 106417150 (DE-625)106417150 AR 15 2005 4 10 448-458 |
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10.1007/BF02892152 doi (DE-627)OLC2051256640 (DE-He213)BF02892152-p DE-627 ger DE-627 rakwb eng 910 VZ 14 ssgn 74.00$jGeographie$jAnthropogeographie: Allgemeines bkl Wei, Zhang verfasserin aut Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer 2005 Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. Zhijiu, Cui aut Jinliang, Feng aut Chaolu, Yi aut Jianqiang, Yang aut Enthalten in Journal of geographical sciences Science in China Press, 2001 15(2005), 4 vom: Okt., Seite 448-458 (DE-627)33352800X (DE-600)2055945-8 (DE-576)094642230 1009-637X nnns volume:15 year:2005 number:4 month:10 pages:448-458 https://doi.org/10.1007/BF02892152 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_4314 74.00$jGeographie$jAnthropogeographie: Allgemeines VZ 106417150 (DE-625)106417150 AR 15 2005 4 10 448-458 |
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10.1007/BF02892152 doi (DE-627)OLC2051256640 (DE-He213)BF02892152-p DE-627 ger DE-627 rakwb eng 910 VZ 14 ssgn 74.00$jGeographie$jAnthropogeographie: Allgemeines bkl Wei, Zhang verfasserin aut Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer 2005 Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. Zhijiu, Cui aut Jinliang, Feng aut Chaolu, Yi aut Jianqiang, Yang aut Enthalten in Journal of geographical sciences Science in China Press, 2001 15(2005), 4 vom: Okt., Seite 448-458 (DE-627)33352800X (DE-600)2055945-8 (DE-576)094642230 1009-637X nnns volume:15 year:2005 number:4 month:10 pages:448-458 https://doi.org/10.1007/BF02892152 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_4314 74.00$jGeographie$jAnthropogeographie: Allgemeines VZ 106417150 (DE-625)106417150 AR 15 2005 4 10 448-458 |
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Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province |
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Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province |
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Wei, Zhang |
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Journal of geographical sciences |
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2005 |
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Wei, Zhang Zhijiu, Cui Jinliang, Feng Chaolu, Yi Jianqiang, Yang |
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late pleistocene glaciation of the hulifang massif of gongwang mountains in yunnan province |
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Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province |
| abstract |
Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. © Springer 2005 |
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Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. © Springer 2005 |
| abstract_unstemmed |
Abstract Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountains constitute one of the typical places once glaciated. Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about 100 ka BP and two TL absolute ages (101,100 ± 7780 a BP; 104,000 ± 8300 a BP) indicate this advance happened during the Penultimate Glaciation. The early stage glacial advance (YJT-II advance) during the last glaciation occurred about 40,920 ± 3400 a BP. The last glacial maximum advance (YJT-III advance) about 18–25 ka BP, which sustained by two TL ages (18,230 ±1420 a BP; 25,420 ± 2110 a BP). The Penultimate and the early stage glaciations were more extensive and the last glacial maximum (LGM) and the late-glacial period (YJT-IV advance, 10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains just like the advances in the western part such as Diancang mountains, Yulong mountains of Yunnan Province and the glacier series are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representative of climate changes during the last glacial cycle in Yunnan Province. © Springer 2005 |
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Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province |
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