Objective

08.01.2013 • Views

Share Embed Flag

Objective

Objective

DOWNLOAD ePAPER

kraut.carlotta49

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

START NOW

Critical Wedge Model<br />

Shape control<br />

Basal friction, strength of the wedge, internal<br />

pore pressure, and fluxes of material.

1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22

å°ç£çæ´»åæ·å±¤

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

Critical Wedge Model Shape control Basal friction, strength of the wedge, internal pore pressure, and fluxes of material.

Critical Wedge Model Strength of wedge Stronger than décollement – flatter wedge Weaker than décollement – steeper wedge

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: Critical Wedge Model α = surface
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!