Results 281 to 290 of about 1,556,019 (343)
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The Alpine Fault, New Zealand: Surface Geology and Field Relationships
, 2013The Alpine Fault forms part of the on-land Pacific-Australian plate boundary. Generally the fault has a simple straight trace, striking ca. 055° and dipping moderately eastwards, but in central areas it is serially partitioned. Late Quaternary strike-slip rates are 23-25 mm/yr, but dip-slip rates range from ca.
R. Norris, A. Cooper
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Looking at fault reactivation matching structural geology and seismological data
Journal of Structural Geology, 2005C. Collettini +4 more
semanticscholar +3 more sources
Fault-related folding: A review of kinematic models and their application
Earth-Science Reviews, 2014C. Brandes, D. Tanner
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Reactivation history of the North Anatolian fault zone based on calcite age-strain analyses
Geology, 2019Perach Nuriel1*, John Craddock2, Andrew R.C. Kylander-Clark3, I. Tonguç Uysal4, Volkan Karabacak5, Ramazan Kadir Dirik6, Bradley R. Hacker3, and Ram Weinberger1,7 1Geological Survey of Israel, 32 Yeshayahu Leibowitz St.
P. Nuriel +7 more
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A review of fault sealing behaviour and its evaluation in siliciclastic rocks
Earth-Science Reviews, 2015Yangwen Pei +3 more
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Geology of the Henty Fault Wedge, Western Tasmania
2023The Henty Fault Wedge is a misfit slice of Cambrian lithologies which have been fault emplaced into the middle to late Cambrian Mt Read Volcanics. The Henty Fault Wedge has an exposed area of 30km\\(^2\\) and is located midway between Queenstown and Rosebery in western Tasmania (Fig 1).
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Looking at fault inversion matching structural geology and seismology
Journal of Structural Geology, 2005Abstract We investigate fault reactivation that occurred during the 1997 Colfiorito seismic sequence (central Italy), matching detailed structural geology, precise earthquake locations and mechanical models of fault interaction. The Colfiorito area, within the Northern Apennines, is characterised by a relatively recent inversion of the tectonic ...
COLLETTINI, Cristiano +4 more
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Quaternary Geology and Faulting in the Damxung‐Yangbajain Basin
Acta Geologica Sinica - English Edition, 2004Abstract The detailed geological mapping, conducted in the Damxung‐Yangbajain basin, shows that there are many types of deposits formed since the Pliocene. The oldest sediments are formed during the Pliocene. The most prominent sediments are three sets of moraines and fluvioglacial deposits.
WU Zhonghai +5 more
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Surficial geology indicates early Holocene faulting and seismicity, central Sweden
International Journal of Earth Sciences, 2014In Sweden, knowledge of the location and timing of glacially induced faulting and seismicity is critical to effective engineering of a long-term nuclear disposal facility. To improve understanding and modeling of the complex ice-induced and tectonic stresses associated with glacially induced faulting, field studies detailing the location and timing of ...
Colby A. Smith +2 more
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