首页/数据集/Geodynamic Evolution of the Proto-Tethys Ocean in the West Kunlun Orogenic Belt, NW Tibet: Implications from the Sub-Arc Crust and Lithospheric Mantle Modification

Geodynamic Evolution of the Proto-Tethys Ocean in the West Kunlun Orogenic Belt, NW Tibet: Implications from the Sub-Arc Crust and Lithospheric Mantle Modification

NIAID Data Ecosystem2026-05-02 收录

构造地质学

地球动力学

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资源简介：

Geodynamic Evolution of the Proto-Tethys Ocean in the West Kunlun Orogenic Belt

应用场景：

创建时间：

2024-09-06

地质年代学

构造地质学

Smeraglia, L., Looser, N., Fabbri, O., Choulet, F., Guillong, M., and Bernasconi, S. M.: U-Pb dating of middle Eocene-middle Pleistocene multiple tectonic pulses in the Alpine foreland, Solid Earth Di

Mendeley Data2024-01-31 更新120

Early Neoproterozoic granitic gneisses in the Amdo micro-continent, Tibet: petrogenesis and geodynamic implications

岩石成因

地球动力学

The palaeogeographic locations of ancient continental blocks in the Tibetan Plateau, especially of micro-continental blocks during the Neoproterozoic supercontinent cycle, remain enigmatic. To clarify

DataCite Commons2025-06-01 更新110

ES-6 – Analytical Results. Segmentation of the Caledonian orogenic infrastructure an exhumation of the Western Gneiss Region during transtensional collapse

构造地质学

造山带地质

ES-6 – Analytical Results (XLS).

Figshare2020-12-16 更新50

羌塘地块白垩纪锆石(U—Th)/He年龄数据

地质年代学

构造地质学

样品为羌科-1井、羌地-17井和羌资-16井。分析测试工作在中国科学院地质与地球物理研究所氩氩、铀—钍—氦年代学实验室完成，测试方法见吴林等(2016)。取得成果如下：青藏高原内部羌塘地块三个钻孔岩芯中9件样品的锆石(U—Th)/He年龄，除始新统两件样品的锆石(U—Th)/He热史信息尚未重置外，其余样品年龄均集中在白垩纪，且年龄值随高程变化较小，指示存在白垩纪剥蚀—冷却。羌塘地块西部 QD-

国家青藏高原科学数据中心2021-06-20 更新120

(U-Th)/He data for manuscript 'Late Oligocene tectonic uplift of the East Kunlun Shan: Expansion of the northeastern Tibetan Plateau'.

地质学

构造地质学

(U-Th)/He data for manuscript 'Late Oligocene tectonic uplift of the East Kunlun Shan: Expansion of the northeastern Tibetan Plateau'.

DataCite Commons2020-10-14 更新60