2004
DOI: 10.1306/04290403092
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Evidence and mechanisms for folding of granite, Sierra de Hualfín basement-cored uplift, northwest Argentina

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Cited by 19 publications
(31 citation statements)
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“…In this case, the backlimb rotation can be attributed to the deformed basement-cover interface and does not require the underlying fault to be listric. In other examples, using field data, Casas et al [2003] and Garcia and Davis [2004] showed that basement blocks surrounding thrust faults deformed during compression. Thus, the shape of a fold does not only depend on the fault geometry, but also on the distribution of the deformation in the cover and the basement rocks.…”
Section: Introductionmentioning
confidence: 99%
“…In this case, the backlimb rotation can be attributed to the deformed basement-cover interface and does not require the underlying fault to be listric. In other examples, using field data, Casas et al [2003] and Garcia and Davis [2004] showed that basement blocks surrounding thrust faults deformed during compression. Thus, the shape of a fold does not only depend on the fault geometry, but also on the distribution of the deformation in the cover and the basement rocks.…”
Section: Introductionmentioning
confidence: 99%
“…Most ranges are bound on at least one side by high angle reverse faults (dips >30°); typically, these are mechanically unsuitable for accommodating slip and require preexisting weaknesses that can be reactivated [ Sibson , ] or assist in their initiation [ Selander et al ., ]. Other ranges consist of broad arch anticlines that developed at upper crustal temperatures by slip on numerous preexisting fractures and discontinuities [ Schmidt et al ., ; Garcia and Davis , ]; these are often interpreted to correspond to blind reverse faults at depth [e.g., Jordan and Allmendinger , ]. Frequently, structures have been reactivated or initiated out of sequence, with deformation not simply propagating into adjacent basins.…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, Anderson and Barnhard (1986) applied Angelier's (1979) García andDavis (2004, Fig. 3b, p. 1260).…”
Section: Regional Stress and Strain Directionsmentioning
confidence: 96%
“…17), perhaps originating as a footwall shortcut on an inverted listric shear zone. Insight into the folding of granite, through trishear fault-propagation folding, was presented by García and Davis (2004Davis ( , p. 1274, based on their analysis of the Sierra de Hualfín basement-cored uplift in the Sierras Pampeanas:…”
Section: Trishear Development Of Colorado Plateau Monoclinesmentioning
confidence: 99%