Acta Geographica Sinica ›› 2016, Vol. 71 ›› Issue (3): 412-421.doi: 10.11821/dlxb201603005
• Geomorphology • Previous Articles Next Articles
Yan DAI1(), Xianyan WANG1(
), Shengli WANG2, Yiquan LI1, Huayu LU1
Received:
2015-11-12
Revised:
2015-12-27
Online:
2016-03-25
Published:
2016-03-25
Supported by:
Yan DAI, Xianyan WANG, Shengli WANG, Yiquan LI, Huayu LU. The neotectonic activity of Wanchuan catchment reflected by geomorphic indices[J].Acta Geographica Sinica, 2016, 71(3): 412-421.
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Tab. 1
The values of the mountain front sinuosity index and the valley floor height-to-width radio index in the Xinglong Mountain and the north of Wanchuan Valley
兴隆山北 | 宛川河北 | ||
---|---|---|---|
SMF | VF | SMF | VF |
1.83 | 0.55 | 1.03 | 0.36 |
1.86 | 1.97 | 1.08 | 0.38 |
2.10 | 1.90 | 1.09 | 0.44 |
2.21 | 2.11 | 1.09 | 0.47 |
2.60 | 4.18 | 1.13 | 0.51 |
2.88 | 5.09 | 1.14 | 0.54 |
7.71 | 1.17 | 0.59 | |
8.46 | 1.18 | 0.65 | |
11.86 | 0.65 | ||
13.00 | 0.81 | ||
0.88 | |||
1.06 | |||
1.05 | |||
2.34 |
Fig. 6
Photos showing the fault scarp and fracture (a. Fault facet at Songjiayao village (east of Gaoya, see location in Fig.1 and Fig. 6d; the lens to the southeast); b. Fault facet at west of Songjiayao village (see location in Fig.6d; the lens to the northeast); c. The cracks on the surface of the Tertiary sandstone in the footwall of the fault (the lens to the surface);d. Fault facet in Google earth image)
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