Late Oligocene to Pleistocene thermo-tectonic evolution of the Karakoram Fault Zone: New insights from basement and detrital apatite fission track thermochronology

The Karakoram Fault Zone displays distinctive topographic and tectonic characteristics, with intricate river drainage systems. Although there are extensive thermochronological datasets for the western Tibetan Plateau, limited investigations have been carried out to uncover the low-temperature therma...

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Veröffentlicht in:Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2024-07, Vol.645, p.112203, Article 112203
Hauptverfasser: Su, Wenbo, Cai, Keda, He, Zhiyuan, Zhao, Xinwei, Zhong, Hua, Glorie, Stijn, De Grave, Johan
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Sprache:eng
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