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- W2390745608 abstract "The thick carbonate was deposited on the foreland of western Kunrin mountain in northwest margin of Tarim basin in Yigeziya Formation of the upper Cretaceous.The distribution of carbonate is from Kashi in the west to Keliyang of Yecheng county in the east.The bioclast limestone is one of the most important lithofacies of eight lithofacies.Oosparite and bioclast sparite are the main compositions of carbonate.The main sedimentary facies are carbonate plateform edge,open carbonate platform and limited carbonate platform.From the west to the east, the evolution of sedimentary environment is from carbonate plateform edge,open carbonate platform to limited carbonate platform.From the west to the east,the thickness of Yigeziya Formation changes from 125 meters to 20 meters.Seven meter scale sychles were recognized in thick carbonate deposition. They are new sequence of oil and gas survey in Cretaceous in Tarim basin. The rich fossils of oyster mactra and spiral shell,carbonate plateform and reef shore show that the north western Tarim basin was sea with the mouth open to the northwest,and the palaeoclimate was warm,the palaeosalinity was salt to semisalt.The palaeosea graphic shape was long narrow band from Tajike in the west to Keliyang of Yecheng county in the east." @default.
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- W2390745608 date "2002-01-01" @default.
- W2390745608 modified "2023-09-25" @default.
- W2390745608 title "The Carbonate Depositional Features of Yigeziya Formation of Upper Cretaceous in Tarim Basin and Their Geological Implication" @default.
- W2390745608 hasPublicationYear "2002" @default.
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