Formation and erosional decay of peneplains in the northern Gandise belt, Tibetan Plateau, revealed by low-temperature thermochronology and cosmogenic nuclides
低温热年代学和宇宙成因核素揭示青藏高原冈底斯带北部准平原的形成和侵蚀衰变
基本信息
- 批准号:69097368
- 负责人:
- 金额:--
- 依托单位:
- 依托单位国家:德国
- 项目类别:Priority Programmes
- 财政年份:2008
- 资助国家:德国
- 起止时间:2007-12-31 至 2013-12-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
Large-scale peneplains constitute the most prominent geomorphic element of the Tibetan Plateau, but little is known about their formation and subsequent evolution. By applying lowtemperature thermochronology, sediment provenance analysis, and cosmogenic nuclides we aim to (1) date the planation phase in south-central Tibet, (2) reconstruct the paleogeography and geologic setting during post-orogenic erosion and basin formation, (3) quantify the Quaternary erosion rate of the low-relief surfaces and the incision rate of rivers dissecting the peneplains, and (4) evaluate whether the peneplains were covered by ice for extended periods in the Quaternary. Our preliminary results suggest that different structural blocks have variable thermal histories. Basement rocks exposed at the peneplains cooled below apatite FT and He closure temperatures (ca. 110 and 70 °C, respectively) between 89 and 35 Ma. 10Be concentrations in granitic bedrock and grus samples yield local erosion rates of 6-12 m Ma-1, whereas catchment-wide erosion rates are only slightly higher (11-18 m Ma-1). This demonstrates that the peneplain region is extremely stable and has barely been modified by erosion in the last millions of years.
我们的初步结果表明,不同的构造块体具有不同的热史。暴露在准平原的基底岩石在磷灰石FT和He闭合温度(分别约110℃和70℃)89 - 35 Ma以下冷却。花岗岩基岩和砾石样品中的be浓度产生了6-12 m Ma-1的局部侵蚀速率,而整个流域的侵蚀速率仅略高(11-18 m Ma-1)。这表明,准平原地区非常稳定,在过去的数百万年里几乎没有受到侵蚀的影响。
项目成果
期刊论文数量(2)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Peneplain formation in southern Tibet predates the India-Asia collision and plateau uplift
- DOI:10.1130/g32069.1
- 发表时间:2011-10-01
- 期刊:
- 影响因子:5.8
- 作者:Hetzel, Ralf;Dunkl, Istvan;Frei, Dirk
- 通讯作者:Frei, Dirk
Cretaceous to Cenozoic evolution of the northern Lhasa Terrane and the Early Paleogene development of peneplains at Nam Co, Tibetan Plateau
- DOI:10.1016/j.jseaes.2013.03.005
- 发表时间:2013-07-01
- 期刊:
- 影响因子:3
- 作者:Haider, Vicky L.;Dunkl, Istvan;Zhang, Liyun
- 通讯作者:Zhang, Liyun
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Dr. István Dunkl其他文献
Dr. István Dunkl的其他文献
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{{ truncateString('Dr. István Dunkl', 18)}}的其他基金
Calibration of carbonaceous material Raman geothermometry and zircon (U-Th)/He thermochronometry for diagenetic to very low-grade metamorphic conditions
成岩至极低级变质条件下碳质材料拉曼地温计和锆石 (U-Th)/He 测温仪的校准
- 批准号:
238775591 - 财政年份:2013
- 资助金额:
-- - 项目类别:
Research Grants
Fluorite (U-Th)/He geochronology: methodical development and case studies
萤石 (U-Th)/He 地质年代学:方法开发和案例研究
- 批准号:
183931056 - 财政年份:2011
- 资助金额:
-- - 项目类别:
Research Grants
How does/did the Tibetan Plateau grow? Geologic-geophysical research in NE-Tibet
青藏高原是如何生长的?
- 批准号:
27726085 - 财政年份:2006
- 资助金额:
-- - 项目类别:
Research Grants
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