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Displacement transfer from fault-bend to fault-propagation fold geometry: An example from the Himalayan thrust front

Creator:

Qayyum, Mazhar, Spratt, Deborah A., Dixon, John M., and Lawrence, Robert D.

Abstract:

The leading edge of the ENE-trending Himalayan thrust front in Pakistan exhibits along-strike changes in deformational style, ranging from fault-bend to fault-propagation folds. Although the structural geometry is very gently deformed throughout the Salt Range, it becomes progressively more complex to the east as the leading edge of the emergent...

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front Mazhar Qayyum a, *, Deborah A. Spratt b, John M. Dixon c, Robert D. Lawrence d a Talisman Energy
Permeability and pressure measurements in Lesser Antilles submarine slides: Evidence for pressure-driven slow-slip failure

Creator:

Hornbach, Matthew J., Manga, Michael, Genecov, Michael, Valdez, Robert, Miller, Peter, Saffer, Demian, Adelstein, Esther, Lafuerza, Sara, Adachi, Tatsuya, Breitkreuz, Christoph, Jutzeler, Martin, Le Friant, Anne, Ishizuka, Osamu, Morgan, Sally, Slagle, Angela, Tailing, Peter J., Fraass, Andrew, Watt, Sebastian F. L., Stroncik, Nicole A., Aljandali, Mohammed, Boudon, Georges, Fujinawa, Akihiko, Hatfield, Robert, Kataoka, Kyoko, Maeno, Fukashi, Martinez-Colon, Michael, McCanta, Molly, Palmer, Martin, Stinton, Adam, Subramanyam, K. S. V., Tamura, Yoshihiko, Villemant, Benoît, Wall-Palmer, Deborah, and Wang, Fei

Abstract:

Recent studies hypothesize that some submarine slides fail via pressure-driven slow-slip deformation. To test this hypothesis, this study derives pore pressures in failed and adjacent unfailed deep marine sediments by integrating rock physics models, physical property measurements on recovered sediment core, and wireline logs. Two drill sites (U1394 and U1399)...

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Article

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, Nicole A. Stroncik14, Mohammed Aljahdali15, Georges Boudon8, Akihiko Fujinawa16, Robert Hatfield17, Kyoko

ScholarsArchive@OSU

Displacement transfer from fault-bend to fault-propagation fold geometry: An example from the Himalayan thrust front

Permeability and pressure measurements in Lesser Antilles submarine slides: Evidence for pressure-driven slow-slip failure

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