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The Chitarwata Formation is a geological formation in western Pakistan, made up of Oligocene and early Miocene terrestrial fluvial facies. The sediments were deposited in coastal depositional environments (estuarine, and tidal flats) when Pakistan was partly covered by the Tethys Ocean. Paleomagnetic data indicates an age range of around 28 to 17 million years ago, with its base in the Oligocene, and its upper boundary, where it meets the overlying , of the Early Miocene.

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  • Chitarwata Formation (en)
  • Formació de Chitarwata (ca)
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  • La Formació de Chitarwata és una formació geològica que es troba al Pakistan occidental originada durant el període de l'Oligocè i del principi del Miocè. Està dominada per paleoambients costaners (estuaris i planes). Les dades paleomagnètiques indiquen que aquesta formació té una edat d'entre 22 a 17 milions d'anys. Junt amb la formació de , la formació de o de la conca de l'Himalaia durant el xoc de les plaques tectòniques de l'Índia i d'Àsia i l'aixecament tectònic de l'Himalaia. (ca)
  • The Chitarwata Formation is a geological formation in western Pakistan, made up of Oligocene and early Miocene terrestrial fluvial facies. The sediments were deposited in coastal depositional environments (estuarine, and tidal flats) when Pakistan was partly covered by the Tethys Ocean. Paleomagnetic data indicates an age range of around 28 to 17 million years ago, with its base in the Oligocene, and its upper boundary, where it meets the overlying , of the Early Miocene. (en)
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  • Chitarwata Formation (en)
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