Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/39582
Title: Igneous sills as a record of horizontal shortening: The San Rafael Subvolcanic Field, Utah
Authors: Walker, R.
Healy, D.
Kawanzaruwa, T. K.
Wright, K.
England, R. W.
McCaffrey, K. J. W.
Bubeck, A. A.
Stephens, T. L.
Farrell, N. J. C.
Blenkinsop, T. G.
First Published: Apr-2017
Publisher: Geological Society of America
Citation: Geological Society of America Bulletin, 2017
Abstract: Igneous sills can facilitate significant lateral magma transport in the crust, therefore it is important to constrain controls on their formation and propagation. Close spatial association between sills and dikes in layered (sedimentary) host rocks has led to a number of sill emplacement mechanisms that involve stress rotation related to layering; from horizontal extension and dike emplacement, to horizontal compression and sill emplacement. Here we use field observations in the San Rafael subvolcanic field (Utah, USA), on the Colorado Plateau, supported by mechanical modelling, to show that layering is not the dominant control in all cases of sill formation. We found no compelling evidence of large sills fed by dikes; all observed cases show that either dikes cut sills, or vice versa. Local sill contacts activate and follow host layer interfaces, but regionally, sills cut the stratigraphy at a low angle. The sills cut and are cut by reverse faults (1-3 m displacement) and related fractures that accommodate horizontal shortening. Minor sill networks resemble extension vein meshes, and indicate that horizontal and inclined geometries were formed during coaxial horizontal shortening and vertical thickening. Although sills elsewhere may be related to mechanical layering during tectonic quiescence, our mechanical models show that the observed SRSVF geometries are favoured in the upper crust during mild horizontal shortening. We propose that sill geometry provides an indication of regional stress states during emplacement, and are not all sill geometry is a response to bedding. Constraining sill geometry may therefore present a useful tool in plate tectonic studies.
DOI Link: 10.1130/B31671.1
ISSN: 0016-7606
eISSN: 1943-2674
Links: http://gsabulletin.gsapubs.org/content/early/2017/04/07/B31671.1.abstract
http://hdl.handle.net/2381/39582
Embargo on file until: 1-May-2018
Version: Post-print
Status: Peer-reviewed
Type: Journal Article
Rights: Copyright © 2017, Geological Society of America. Deposited with reference to the publisher’s open access archiving policy.
Description: The file associated with this record is under embargo until 12 months after publication, in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.
Appears in Collections:Published Articles, Dept. of Geology

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GSAB2016_figures_rev1_reduced.pdfPost-review (final submitted author manuscript)11.15 MBAdobe PDFView/Open
Walker_etal_SRSVF_GSAB_DEC16_FIN.pdfPost-review (final submitted author manuscript)599.97 kBAdobe PDFView/Open


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