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- W2383419683 abstract "Reef complexes of the Lianglitag Formation(Katian,Upper Ordovician)in the Well Block Tazhong 16,Central Tarim High,Tarim Block,NW China are representatives of the evolutionary units of Ordovician reefs.The Lianglitag Formation is composed of five lithological members.The Well Block Tazhong 16is assigned to the ramp belt of the Tazhong Slopebreak I,where the water depth and current energy played significant role for the sedimentary pattern of the carbonate lithofacies.Typical metazoanal reefs are concentrated along the high-energy belt of the platform margin.In contrast,the Well Block Tazhong 16isn't characterized by the reef thriving realm.Lower energy sediments especially lime flats are commonly occurred from the lower members of the formation in the wells of Tazhong 16and 166.Facies of the high-energy bank,carbonate mudmounds as well as reef-surrounding sediments are richly yielded from the upper members.Therefore,it could be considered as the extension area of the large metazoanl reefs from the platform margin toward interior platform.Water depth and current energy are diverse herein.The wells in the northwest part were uplifted earlier since the forming of the Member 2,however,Well Tazhong 161at the southeastward maintained a submarine environment and resulted in the uppermost unit of the Member 1." @default.
- W2383419683 created "2016-06-24" @default.
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- W2383419683 date "2014-01-01" @default.
- W2383419683 modified "2023-09-23" @default.
- W2383419683 title "SEDIMENTARY FACIES OF THE LATE ORDOVICIAN LIANGLITAG FORMATION IN THE WELL BLOCK TAZHONG 16,CENTRAL TARIM,NW CHINA" @default.
- W2383419683 hasPublicationYear "2014" @default.
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