File:Fig4-Geomorphic-expressions-of-normal-faults-near-the-southeast-flank-of-Mt.gif
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English: Fig. 4 Geomorphic expressions of normal faults near the southeast flank of Mt. Kinabalu and the Ranau Basin. Red dashed line shows active fault trace inferred from geomorphology, with up-thrown side marked by U and downthrown side marked by D. Blue-colored arrow indicates the flow direction of channel in the Ranau Basin. The only normal fault that dipping northwestward in this map is the Marakau Fault at the eastern edge of the Ranau Basin. Tri: Triangular facets; Wine: Wineglass canyon; Scr: Scarp; W: Wind gap; BR: Broken ridge. Black contour interval is 50 m, gray contour interval is 10 m |
| Date | |
| Source | Yu Wang et. al. "The 2015 M w 6.0 Mt. Kinabalu earthquake: an infrequent fault rupture within the Crocker fault system of East Malaysia", Geoscience Letters doi:10.1186/s40562-017-0072-9 |
| Author | Yu Wang, Shengji Wei, Xin Wang, Eric O. Lindsey, Felix Tongkul, Paul Tapponnier, Kyle Bradley, Chung-Han Chan, Emma M. Hill, Kerry Sieh |
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Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License ( https://creativecommons.org/licenses/by/4.0/ ), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. |
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| current | 09:47, 4 March 2020 | | 784 × 517 (383 KB) | Sohmen (talk | contribs) | Uploaded by the NOA Upload Tool |
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