Objective

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Objective

Objective

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3D model<br />

Model 3:<br />

weaker material +<br />

enhanced erosion<br />

Close to the condition<br />

of western Taiwan<br />

Topographic<br />

embayment is at least<br />

1000 m

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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

3D model Model 2: enhanced erosion Broad effect on the wedge kinematics Strong erosion controls over the internal organization strain

3D model Model 3: weaker material + enhanced erosion Close to the condition of western Taiwan Topographic embayment is at least 1000 m

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 and 8: Introduction A: north of Tuntzuchi
Page 9 and 10: Critical Wedge Model α = surface
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: 3D model Model 1: weaker material
Page 21 and 22: Discussion Early stage: foreland t
Page 23:
Thank you!