Cooling and denudation history of Spitsbergen, and inferences for tectonics, climate and longterm landscape evolution

斯匹次卑尔根岛的冷却和剥蚀历史以及构造、气候和长期景观演化的推论

• 批准号: 164682497
• 负责人: Professor Dr. Frank Lisker
• 金额: --
• 依托单位: Fachgebiet Geodynamik der Polargebiete
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2010
• 资助国家: 德国
• 起止时间: 2009-12-31 至 2012-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/164682497?language=en
• 关键词: Cooling; denudation; history; Spitsbergen; inferences

This proposal applies for 18 months final funding of a PhD position within a research project in Spitsbergen that is carried out as a cooperation between the Universität Bremen, the Federal Institute for Geosciences and Natural Resources (BGR), and other partners. The project applies apatite fission track (FT) and (U-Th-Sm)/He thermochronology, clay mineral and vitrinite reflectance analysis for reconstructing the thermal history of basement rocks and sedimentary cover. The principle aim of this research is to investigate the Phanerozoic crustal dynamics of northern and central Spitsbergen, its implications on the opening of the Atlantic and consequences on regional long-term climate evolution. Four specific objectives are:1) Passive margin evolution of Svalbard2) Late Mesozoic and Cenozoic regional tectonic history3) Thermal evolution of the Central Tertiary Basin4) Coupling of Neogene climate change and tectonics, and long-term landscape evolution.

该提案适用于斯匹次卑尔根岛一个研究项目的 18 个月的最终资助，该项目是不来梅大学、联邦地球科学和自然资源研究所 (BGR) 和其他合作伙伴合作开展的。该项目应用磷灰石。裂变径迹 (FT) 和 (U-Th-Sm)/He 热年代学、粘土矿物和镜质体反射率分析，用于重建基岩和沉积盖层的热历史 本研究的主要目的是。研究斯匹次卑尔根岛北部和中部的显生宙地壳动力学、其对大西洋开放的影响以及对区域长期气候演化的影响，有四个具体目标：1）斯瓦尔巴群岛的被动边缘演化2）晚中生代和新生代区域构造历史3。 ) 中央第三纪盆地的热演化4) 新近纪气候变化与构造的耦合以及长期地貌演化。

项目成果

Why is Svalbard an island? Evidence for two‐stage uplift, magmatic underplating, and mantle thermal anomalies

• DOI: 10.1002/tect.20039
• 发表时间: 2013-06
• 期刊: Tectonics
• 影响因子: 4.2
• 作者: N. Dörr;P. Clift;F. Lisker;C. Spiegel