Neogene rock uplift and erosion in northern Borneo: Evidence from the Kinabalu granite, Mount Kinabalu
Thermochronological data from the Kinabalu granite, emplaced between c. 7.2 and 7.8 Ma, provide a unique record of northern Borneo's exhumation during the Neogene. Biotite 40Ar/39Ar ages (c. 7.32-7.63 Ma) record rapid cooling of the granite in the Late Mi
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|Source:||Journal of the Geological Society|
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