Climate Change Data Portal
DOI | 10.1002/esp.1380 |
Erosion in northwest Tibet from in-situ-produced cosmogenic Be-10 and Al-26 in bedrock | |
Kong, Ping; Na, Chunguang; Fink, David; Ding, Lin; Huang, Feixin | |
发表日期 | 2007 |
ISSN | 0197-9337 |
EISSN | 1096-9837 |
起始页码 | 116 |
结束页码 | 125 |
卷号 | 32期号:1 |
英文摘要 | Concentrations of in-situ-produced cosmogenic nuclides Be-10 and Al-26 in quartz were measured by accelerator mass spectrometry for bedrock basalts and sandstones located in northwest Tibet. The effective exposure ages range between 23 and 134 ka (Be-10) and erosion rates between 4.0 and 24 mm ka(-1). The erosion rates are significantly higher than those in similarly and Antarctica and Australia, ranging between 0.1 and 1 mm ka(-1), suggesting that precipitation is not the major control of erosion of landforms. Comparison of erosion rates in and regions with contrasting tectonic activities suggests that tectonic activity plays a more important role in controlling long-term erosion rates. The obtained erosion rates are, however, significantly lower than the denudation rate of 3000-6000 mm ka(-1) beginning at c. 53 Ma in the nearby Godwin Austen (K2) determined by apatite fission-track thermochronology. It appears that the difference in erosion rates within different time intervals is indicative of increased tectonic activity at c. 5-3 Ma in northwest Tibet. We explain the low erosion rates determined in this study as reflecting reduced tectonic activity in the last million years. A model of localized thinning of the mantle beneath northwest Tibet may account for the sudden increased tectonic activity at c. 5-3 Ma and the later decrease. Copyright (c) 2006 John Wiley & Sons, Ltd. |
关键词 | PRODUCTION-RATESGLOBAL CLIMATESEDIMENT PRODUCTIONICE-SHEETUPLIFTEVOLUTIONPLATEAUAUSTRALIAVOLCANISMISOTOPES |
英文关键词 | erosion rate; cosmogenic nuclide; northwest Tibet; uplift; tectonics |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000243696000009 |
来源期刊 | EARTH SURFACE PROCESSES AND LANDFORMS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257481 |
推荐引用方式 GB/T 7714 | Kong, Ping,Na, Chunguang,Fink, David,et al. Erosion in northwest Tibet from in-situ-produced cosmogenic Be-10 and Al-26 in bedrock[J]. 中国科学院青藏高原研究所,2007,32(1). |
APA | Kong, Ping,Na, Chunguang,Fink, David,Ding, Lin,&Huang, Feixin.(2007).Erosion in northwest Tibet from in-situ-produced cosmogenic Be-10 and Al-26 in bedrock.EARTH SURFACE PROCESSES AND LANDFORMS,32(1). |
MLA | Kong, Ping,et al."Erosion in northwest Tibet from in-situ-produced cosmogenic Be-10 and Al-26 in bedrock".EARTH SURFACE PROCESSES AND LANDFORMS 32.1(2007). |
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