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The Lameta Formation, also known as the Infratrappean Beds, is a sedimentary geological formation found in Madhya Pradesh, Gujarat, and Maharashtra, India, associated with the Deccan Traps. It is of Maastrichtian age (Late Cretaceous), and is notable for its dinosaur fossils. Many dubious names have been created for isolated bones, but several genera of dinosaurs from these rocks are well-supported, including the titanosaur sauropod Isisaurus and the abelisaurs Indosaurus, Indosuchus, Laevisuchus, and Rajasaurus. As well as mammals, snakes and other fossils.

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  • Souvrství Lameta (cs)
  • Formation de Lameta (fr)
  • Formasi Lameta (in)
  • Lameta Formation (en)
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  • The Lameta Formation, also known as the Infratrappean Beds, is a sedimentary geological formation found in Madhya Pradesh, Gujarat, and Maharashtra, India, associated with the Deccan Traps. It is of Maastrichtian age (Late Cretaceous), and is notable for its dinosaur fossils. Many dubious names have been created for isolated bones, but several genera of dinosaurs from these rocks are well-supported, including the titanosaur sauropod Isisaurus and the abelisaurs Indosaurus, Indosuchus, Laevisuchus, and Rajasaurus. As well as mammals, snakes and other fossils. (en)
  • Formasi Lameta adalah formasi geologi yang terdiri dari batu sedimen dan berasal dari Zaman Kapur akhir, terletrak di negara-negara bagian Madhya Pradesh, Gujarat dan Maharashtra, India dan dikenal karena banyaknya yang ditemukan di sana. Contoh genus dinosaurus yang telah ditemukan dan diidentifikasi dengan jelas diantaranya , suatu sauropoda dari kelompok serta beberapa theropoda dari kelompok : , , dan Rajasaurus. (in)
  • La Formation de Lameta est une formation de roches sédimentaires située dans les régions de Madhya Pradesh, Gujarat et Maharashtra en Inde. Elle est d'âge Maastrichtien (le dernier étage du Crétacé supérieur) daté de −72 à −66 Ma (millions d'années). La Formation de Lameta est connue pour les fossiles de dinosaures qu'elle contient. Beaucoup de noms douteux ont été créés pour des os isolés, mais plusieurs genres de dinosaures trouvés dans ces roches sont bien documentés, comme le titanosaure sauropode Isisaurus et les abelisauridés Indosaurus, Indosuchus, Laevisuchus et Rajasaurus. (fr)
  • Souvrství Lameta je jednou z nejznámějších paleontologických formací s množstvím významných lokalit z období pozdní křídy na území současné Indie. Sedimenty této formace mají stáří asi 70 až 66 milionů let (věk maastricht, nejpozdnější křída) a jejich mocnost činí obvykle 18 až 45 metrů. Rozkládají se na ploše kolem 5000 km² a navazují na výlevné sedimenty tzv. dekkánských trapů (mohutná vulkanická provincie). Vznikaly z větší části v říčním a jezerním prostředí. V době vzniku hornin tohoto souvrství zde panovalo horké a tropické až sušší, spíše semiaridní prostředí. (cs)
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  • Lameta Formation (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Rajasaurus_restoration.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Indosuchus.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Isisaurus_DB.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Rahiolisaurus_restoration.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Sanajeh_attacking_sauropod.png
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