Sedimentary environments of the early Pliocene Ailioachioa ...

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Various magnitude of storm can form different thick of storm beds in same environment.
The symmetric bedform of climbing ripple maybe formed during storm.
Page 1 and 2: Sedimentary environments of the ear
Page 3 and 4: Introduction • The objective of t
Page 5 and 6: Study area Study area Tseng Weng ri
Page 7 and 8: Hoku Hsi section Hoku river section
Page 9 and 10: Outcrop observation • Describe li
Page 11 and 12: Results • Facies and facies assoc
Page 13 and 14: Facies association
Page 27 and 28: Reconstruction of paleo-environment
Page 29: Discussion • The absence of biotu
Page 33 and 34: • The environment in Lower part o
Page 35 and 36: Feature work • Field work ! Go to
Page 37: Maopu Shale Ailioachioa Formation Y

Sedimentary environments of the early Pliocene Ailioachioa ...

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