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Paper No. 1
Presentation Time: 1:30 PM

ADVANCES IN DATA-RICH BALANCING FOR DEEP INSIGHT, WITH EXAMPLES OF RAPIDLY GROWING STRUCTURES IN WESTERN TAIWAN


SUPPE, John1, GRAVELEAU, Fabien2, MARC, Odin3, HUANG, Shiuh-Tsann4 and LE BÉON, Maryline1, (1)Department of Geosciences, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, P.O. Box 13-318, Taipei, 10617, Taiwan, (2)Géosystèmes Lille, Université de Lille 1, FRE 3298 Bât SN5, Avenue Paul Langevin, Villeneuve d'Ascq, 59655, France, (3)Laboratoire de Géologie, Ecole Normale Supérieure, 24 Rue Lhomond, Paris, 75231, France, (4)Exploration and Research Division, CPC Corporation, Miaoli, 36042, Taiwan, suppe@princeton.edu

The classical balancing measurements of area of relief and bed-length that were pioneered by Chamberlin, Laubscher and Epard & Groshong provide a straightforward route to rich structural insight when they are combined with new concepts and rich data from seismic imaging, velocity analysis, well logs and, in the case of active structures, geodesy. These new methods (Gonzalez-Mieres & Suppe 2006, 2010) yield reflector-by-reflector measurements of total shortening, shortening history, and components of shortening, including flexural, pure shear, simple shear and horizontal compaction. The potential sources of error include distortions of imperfect seismic imaging, such as incorrect migration, and failure to properly distinguish stratigraphic and structural thickness variations, but new methods and better data overcome these issues. We illustrate the application of these methods and concepts with two actively growing examples from western Taiwan: [1] Tungshih anticline which is a complex detachment fold that grew by ~10-12 m in the 1999 M=7.6 Chi-Chi earthquake by a combination of kink-band migration and limb rotation and [2] Tainan anticline which is shear fault-bend fold growing in creep by limb rotation above the frontal backthrust of SW Taiwan, currently shortening at ~15 mm/y.
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