Djadochta Formation oor Spaans

Djadochta Formation

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Formación de Djadochta

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Nemegt Basin Nemegt Formation Barun Goyot Formation Djadochta Formation Barsbold, Rinchen (1983): O ptich'ikh chertakh v stroyenii khishchnykh dinozavrov. .
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It is known from a partial skeleton including the skull collected at Alag Teg locality, from the Campanian Djadochta Formation of southern Mongolia.
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Such large river channels and soil deposits are evidence of a far more humid climate than those found in the older Barun Goyot and Djadochta formations.
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Similarly, the Cretaceous Mongolia sequence (which took place during the third episode) was set in the Wulansuhai Formation rather than the near-contemporary, and more familiar, Djadochta Formation.
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The main geological formations in the area are the Nemegt Formation, Barun Goyot Formation, and Djadochta Formation, in order of age, from youngest (most superficial) to oldest (deepest).
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Nemegt sediments preserve large river channels and soil deposits that indicate a far more humid climate than those suggested by the underlying Barun Goyot and Djadochta Formations.
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The main geological formations in the area are the Nemegt Formation, Barun Goyot Formation and Djadochta Formation, in order of age, from youngest (most superficial) to oldest (deepest).[3][4]
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Tarbosaurus is found chiefly in the Nemegt Formation, whose sediments preserve large river channels and soil deposits that indicate a far more humid climate than those suggested by the underlying Barun Goyot and Djadochta Formations.
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