Objective

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Objective

Objective

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Critical Wedge Model<br />

α = surface slope<br />

β = dip of décollement

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Biostratigraphy: time scales from graphic and quantitative methods

Sedimentary environments of the early Pliocene Ailioachioa ...

Seismic Study of the Chaochou Structure, Pingtung, Taiwan

Deposits

SEM Operation: 1. Use Carbon tape or copper tap or carbon ...

10. Seismic Stratigraphy

9. Sequence Stratigraphy

Introduction Synorogenic strata – Kcl – thickness different Cs – uniform thickness Cl、Tk – abrupt change in thickness

Critical Wedge Model α = surface slope β = dip of décollement

Page 1 and 2: Presenter: Ting-Hsuan Hsu 2012/10/4
Page 3 and 4: Introduction OUTLINE Critical Wedg
Page 5 and 6: Introduction Puli Topographic Emba
Page 7: Introduction A: north of Tuntzuchi
Page 11 and 12: Critical Wedge Model Strength of w
Page 13 and 14: Subcritical state? Definition Surfa
Page 15 and 16: Subcritical state? “Negative tape
Page 17 and 18: 3D model Model 1: weaker material
Page 19 and 20: 3D model Model 3: weaker material
Page 21 and 22: Discussion Early stage: foreland t
Page 23:
Thank you!