The rise and demise of the Paleogene Central Tibetan Valley
Reconstructing the Paleogene topography and climate of central Tibet informs
understanding of collisional tectonic mechanisms and their links to climate and biodiversity.
Radiometric dates of volcanic/sedimentary rocks and paleotemperatures based on clumped
isotopes within ancient soil carbonate nodules from the Lunpola Basin, part of an east-west
trending band of basins in central Tibet and now at 4.7 km, suggest that the basin rose from<
2.0 km at 50 to 38 million years (Ma) to> 4.0 km by 29 Ma. The height change is quantified …
understanding of collisional tectonic mechanisms and their links to climate and biodiversity.
Radiometric dates of volcanic/sedimentary rocks and paleotemperatures based on clumped
isotopes within ancient soil carbonate nodules from the Lunpola Basin, part of an east-west
trending band of basins in central Tibet and now at 4.7 km, suggest that the basin rose from<
2.0 km at 50 to 38 million years (Ma) to> 4.0 km by 29 Ma. The height change is quantified …
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