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paleostress

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Journal Article
Journal: Geology
Published: 04 January 2018
Geology (2018) 46 (3): 195-198.
... Ridge of central Virginia (USA). The widespread presence of these CPOs in minimally deformed quartz rocks suggests that they may be useful in defining paleostress trajectories. 04 08 2017 17 11 2017 19 11 2017 © 2018 Geological Society of America 2018 The alignment...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.4
EISBN: 9781786203410
FIGURES | View All (12)
Series: Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP421.8
EISBN: 9781862399549
FIGURES | View All (14)
Series: GCSSEPM
Published: 01 January 2014
DOI: 10.5724/gcs.14.33.0415
EISBN: 978-0-9836097-9-0
... Abstract We compiled paleostress analyses from previous research works collected at 591 localities of striated fault planes in rocks ranging in age from Late Cretaceous to Quaternary in the circum-Caribbean and Mexico. The purpose of the study is to quantify a progressive clockwise rotation...
Series: GSA Special Papers
Published: 01 August 2013
DOI: 10.1130/2013.2497(14)
Series: GSA Special Papers
Published: 01 April 2013
DOI: 10.1130/2013.2494(14)
... on these fault measurements and paleostresses computed from them. (1) Compared to the typical northerly striking normal to normal-oblique faults in the rift basins to the north and south, normal-oblique faults are broadly distributed within two merging, NE-trending zones on the northwest and southeast sides...
Series: GSA Field Guide
Published: 01 January 2013
DOI: 10.1130/2013.0033(03)
EISBN: 9780813756332
..., lithology, and fault strength led to curved thrust slip and differential shortening. Within the Laramide foreland, structural styles of basement-cored arches, sedimentation in basins, paleostress/strain patterns, and combined AMS and paleomagnetism of red beds are examined to test models of foreland...
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Journal Article
Published: 01 June 1982
Journal of the Geological Society (1982) 139 (3): 293-297.